Hostname: page-component-76fb5796d-45l2p Total loading time: 0 Render date: 2024-04-28T00:42:47.386Z Has data issue: false hasContentIssue false
  • English
  • Français

How the geochemistry of syn-kinematic calcite cement depicts past fluid flow and assists structural interpretations: a review of concepts and applications in orogenic forelands

Published online by Cambridge University Press:  15 February 2023

Nicolas E. Beaudoin Open the ORCID record for Nicolas E. Beaudoin [Opens in a new window] ,
Olivier Lacombe ,
Guilhem Hoareau  and
Jean-Paul Callot
Nicolas E. Beaudoin*
Affiliation:
Universite de Pau et des Pays de l’Adour, E2S UPPA, LFCR, CNRS, Total Energies, Pau, France
Olivier Lacombe
Affiliation:
Sorbonne Université, CNRS-INSU, Institut des Sciences de la Terre de Paris – ISTeP, UMR7193, Paris, France
Guilhem Hoareau
Affiliation:
Universite de Pau et des Pays de l’Adour, E2S UPPA, LFCR, CNRS, Total Energies, Pau, France
Jean-Paul Callot
Affiliation:
Universite de Pau et des Pays de l’Adour, E2S UPPA, LFCR, CNRS, Total Energies, Pau, France
*
Author for correspondence: Nicolas E. Beaudoin, Email: nicolas.beaudoin@univ-pau.fr
Get access Rights & Permissions [Opens in a new window]

Abstract

Orogenic forelands host interactions between deformation and static or migrating fluids. Given their accessibility and dimensions, these areas are not only historic landmarks for structural geology, but they are also areas of prime interest for georesource exploration and geological storage, and loci of potential geohazards. Geochemical techniques applied on cements filling tectonic structures and associated trapped fluids can constrain the temperature, pressure, origin and pathways of fluids during deformation and allow the characterization of the past fluid system. In this review focused on calcite cements, we first present and critically discuss the most used geochemical techniques to appraise specific parameters of the fluid system. Second, we summarize the outcomes of selected case studies where the past fluid system was reconstructed with consideration of tectonics, either at the scale of the individual fold/thrust or at the scale of the fold-and-thrust belt. At first order, the past fluid system evolves in a similar way with respect to the considered stage of deformation, being rather closed to external fluids when deformation is bounded to mesoscale structure development, and opening to vertical flow when thrust and folds develop. In a more detailed view, it seems that the past fluid system evolves and distributes under the influence of the structural style, of the geometry of the major faults and of the lithology of the sedimentary succession. Through this review, we illustrate the concept of geochemistry-assisted structural geology through case studies where the geochemistry of calcite veins constrained subsurface geometries and structural developments in orogenic forelands.

Keywords

fold-and-thrust beltsfluid flowgeochemistrystructural geologyreviewfractures
Type
FLUID FLOW AND MINERALIZATION IN FAULTS AND FRACTURES
Information
Geological Magazine , Volume 159 , Issue 11-12: THEMATIC ISSUE: Faults and fractures in rocks: mechanics, occurrence, dating, stress history and fluid flow , November 2022 , pp. 2157 - 2190
Copyright
© The Author(s), 2023. Published by Cambridge University Press

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Accaino, F, Bratus, A, Conti, S, Fontana, D and Tinivella, U (2007) Fluid seepage in mud volcanoes of the northern Apennines: an integrated geophysical and geological study. Journal of Applied Geophysics 63, 90–101.CrossRefGoogle Scholar
Affek, HP (2012) Clumped isotope paleothermometry: principles, applications, and challenges. The Paleontological Society Papers 18, 101–14.CrossRefGoogle Scholar
Affolter, S, Fleitmann, D and Leuenberger, M (2014) New online method for water isotope analysis of speleothem fluid inclusions using laser absorption spectroscopy (WS-CRDS). Climate of the Past 10, 1291–304.CrossRefGoogle Scholar
Agosta, F (2008) Fluid flow properties of basin-bounding normal faults in platform carbonates, Fucino Basin, central Italy. In The Geodynamics of the Aegean and Anatolia (eds T Taymaz, Y Yilmaz and Y Dilek), pp. 277–91. Geological Society of London, Special Publication no. 299.CrossRefGoogle Scholar
Agosta, F and Kirschner, DL (2003) Fluid conduits in carbonate-hosted seismogenic normal faults of central Italy. Journal of Geophysical Research: Solid Earth 108, 2221.CrossRefGoogle Scholar
Agosta, F, Luetkemeyer, PB, Lamarche, J, Crider, JG and Lacombe, O (2016) An introduction to the Special Issue on “The role of fluids in faulting and fracturing in carbonates and other upper crustal rocks”. Tectonophysics 690, 1–3.CrossRefGoogle Scholar
Aharonov, E and Karcz, Z (2019) How stylolite tips crack rocks. Journal of Structural Geology 118, 299–307.CrossRefGoogle Scholar
Ahmadhadi, F, Lacombe, O and Daniel, JM (2007) Early reactivation of basement faults in Central Zagros (SW Iran): evidence from pre-folding fracture populations in the Asmari Formation and Lower Tertiary paleogeography. In Thrust Belts and Foreland Basins: From Fold Kinematics to Hydrocarbon Systems (eds Lacombe, O, Lavé, J, Vergés, J and Roure, F), pp. 205–28. Berlin: Springer-Verlag.CrossRefGoogle Scholar
Al-Aasm, I, Lonnee, J and Clarke, J (2000) Multiple fluid flow events and the formation of saddle dolomite: examples from Middle Devonian carbonates of the Western Canada Sedimentary Basin. Journal of Geochemical Exploration 69–70, 11–5.CrossRefGoogle Scholar
Al-Aasm, IS, Lonnee, J and Clarke, J (2002) Multiple fluid flow events and the formation of saddle dolomite: case studies from the Middle Devonian of the Western Canada Sedimentary Basin. Marine and Petroleum Geology 19, 209–17.CrossRefGoogle Scholar
Amrouch, K, Beaudoin, N, Lacombe, O, Bellahsen, N and Daniel, J-M (2011) Paleostress magnitudes in folded sedimentary rocks. Geophysical Research Letters 38, L17301.CrossRefGoogle Scholar
Amrouch, K, Lacombe, O, Bellahsen, N, Daniel, JM and Callot, JP (2010b) Stress and strain patterns, kinematics and deformation mechanisms in a basement-cored anticline: Sheep Mountain Anticline, Wyoming. Tectonics 29, TC1005.CrossRefGoogle Scholar
Amrouch, K, Robion, P, Callot, JP, Lacombe, O, Daniel, JM, Bellahsen, N and Faure, JL (2010a) Constraints on deformation mechanisms during folding provided by rock physical properties: a case study at Sheep Mountain anticline (Wyoming, USA). Geophysical Journal International 182, 1105–23.CrossRefGoogle Scholar
Andersen, MB, Stirling, CH, Potter, E-K, Halliday, AN, Blake, SG, McCulloch, MT, Ayling, BF and O’Leary, M (2008) High-precision U-series measurements of more than 500,000 year old fossil corals. Earth and Planetary Science Letters 265, 229–45.CrossRefGoogle Scholar
Anderson, NT, Kelson, JR, Kele, S, Daëron, M, Bonifacie, M, Horita, J, Mackey, TJ, John, CM, Kluge, T, Petschnig, P, Jost, AB, Huntington, KW, Bernasconi, SM and Bergmann, KD (2021) A unified clumped isotope thermometer calibration (0.5–1,100°C) using carbonate-based standardization. Geophysical Research Letters 48, e2020GL092069.CrossRefGoogle Scholar
André, AS, Sausse, J and Lespinasse, M (2001) New approach for the quantification of paleostress magnitudes: application to the Soultz vein system (Rhine graben, France). Tectonophysics 336, 215–31.CrossRefGoogle Scholar
Andresen, KJ (2012) Fluid flow features in hydrocarbon plumbing systems: what do they tell us about the basin evolution? Marine Geology 332, 89–108.CrossRefGoogle Scholar
Archie, GE (1952) Classification of carbonate reservoir rocks and petrophysical considerations. AAPG Bulletin 36, 278–98.Google Scholar
Arndt, M, Virgo, S, Cox, SF and Urai, JL (2014) Changes in fluid pathways in a calcite vein mesh (Natih Formation, Oman Mountains): insights from stable isotopes. Geofluids 14, 391–418.CrossRefGoogle Scholar
Aubert, I, Léonide, P, Lamarche, J and Salardon, R (2020) Diagenetic evolution of fault zones in Urgonian microporous carbonates, impact on reservoir properties (Provence – Southeast France). Solid Earth 11, 1163–86.CrossRefGoogle Scholar
Baietto, A, Cadoppi, P, Martinotti, G, Perello, P, Perrochet, P and Vuataz, FD (2008) Assessment of thermal circulations in strike-slip fault systems: the Terme di Valdieri case (Italian western Alps). In The Geodynamics of the Aegean and Anatolia (eds T Taymaz, Y Yilmaz and Y Dilek), pp. 317–39. Geological Society of London, Special Publication no. 299.CrossRefGoogle Scholar
Bakker, RJ (2003) Package FLUIDS 1. Computer programs for analysis of fluid inclusion data and for modelling bulk fluid properties. Chemical Geology 194, 3–23.CrossRefGoogle Scholar
Ballentine, CJ and Burnard, PG (2002). Production, release and transport of noble gases in the continental crust. Reviews in Mineralogy and Geochemistry 47, 481–538.CrossRefGoogle Scholar
Bar, E, Nuriel, P, Kylander-Clark, A and Weinberger, R (2021) Towards in situ U-Pb dating of dolomite. Geochronology 3, 337–49.Google Scholar
Barbier, M, Floquet, M, Hamon, Y and Callot, JP (2015) Nature and distribution of diagenetic phases and petrophysical properties of carbonates: the Mississippian Madison Formation (Bighorn Basin, Wyoming, USA). Marine and Petroleum Geology 67, 230–48.CrossRefGoogle Scholar
Barbier, M, Hamon, Y, Callot, JP, Floquet, M and Daniel, JM (2012b) Sedimentary and diagenetic controls on the multiscale fracturing pattern of a carbonate reservoir: the Madison Formation (Sheep Mountain, Wyoming, USA). Marine and Petroleum Geology 29, 50–67.CrossRefGoogle Scholar
Barbier, M, Leprêtre, R, Callot, JP, Gasparrini, M, Daniel, JM, Hamon, Y, Lacombe, O and Floquet, M (2012a) Impact of fracture stratigraphy on the paleo-hydrogeology of the Madison Limestone in two basement-involved folds in the Bighorn basin, (Wyoming, USA). Tectonophysics 576–577, 116–32.CrossRefGoogle Scholar
Barker, SL, Cox, SF, Eggins, SM and Gagan, MK (2006) Microchemical evidence for episodic growth of antitaxial veins during fracture-controlled fluid flow. Earth and Planetary Science Letters 250, 331–44.CrossRefGoogle Scholar
Barker, SLL, Bennett, VC, Cox, SF, Norman, MD and Gagan, MK (2009) Sm–Nd, Sr, C and O isotope systematics in hydrothermal calcite–fluorite veins: implications for fluid–rock reaction and geochronology. Chemical Geology 268, 58–66.CrossRefGoogle Scholar
Bau, M and Möller, P (1993) Rare earth element systematics of the chemically precipitated component in early Precambrian iron formations and the evolution of the terrestrial atmosphere-hydrosphere-lithosphere system. Geochimica et Cosmochimica Acta 57, 2239–49.CrossRefGoogle Scholar
Beaudoin, N, Bellahsen, N, Lacombe, O and Emmanuel, L (2011) Fracture-controlled paleohydrogeology in a basement-cored, fault-related fold: Sheep Mountain Anticline, Wyoming, United States. Geochemistry, Geophysics, Geosystems 12, Q06011.CrossRefGoogle Scholar
Beaudoin, N, Bellahsen, N, Lacombe, O, Emmanuel, L and Pironon, J (2014a) Crustal-scale fluid flow during the tectonic evolution of the Bighorn Basin (Wyoming, USA). Basin Research 26, 403–35.CrossRefGoogle Scholar
Beaudoin, N and Lacombe, O (2018) Recent and future trends in paleopiezometry in the diagenetic domain: insights into the tectonic paleostress and burial depth history of fold-and-thrust belts and sedimentary basins. Journal of Structural Geology 114, 357–65.CrossRefGoogle Scholar
Beaudoin, N, Lacombe, O, Bellahsen, N, Amrouch, K and Daniel, J-M (2014b) Evolution of pore-fluid pressure during folding and basin contraction in overpressured reservoirs: insights from the Madison-Phosphoria carbonate formations in the Bighorn Basin (Wyoming, USA). Marine and Petroleum Geology 55, 214–29.CrossRefGoogle Scholar
Beaudoin, N, Lacombe, O, Bellahsen, N and Emmanuel, L (2013) Contribution of studies of sub-seismic fracture populations to paleo-hydrological reconstructions (Bighorn Basin, USA). Procedia Earth and Planetary Science 7, 57–60.CrossRefGoogle Scholar
Beaudoin, N, Leprêtre, R, Bellahsen, N, Lacombe, O, Amrouch, K, Callot, J-P, Emmanuel, L and Daniel, J-M (2012) Structural and microstructural evolution of the Rattlesnake Mountain Anticline (Wyoming, USA): new insights into the Sevier and Laramide orogenic stress build-up in the Bighorn Basin. Tectonophysics 576–577, 20–45.CrossRefGoogle Scholar
Beaudoin, G and Therrien, P (2004) The web stable isotope fractionation calculator. In Handbook of Stable Isotope Analytical Techniques, (ed P. de Groot), Elsevier pp. 1045–48.CrossRefGoogle Scholar
Beaudoin, N, Gasparrini, M, David, ME, Lacombe, O and Koehn, D (2019b) Bedding-parallel stylolites as a tool to unravel maximum burial depth in sedimentary basins: application to Middle Jurassic carbonate reservoirs in the Paris basin. Geological Society of America Bulletin 131, 1239–54.CrossRefGoogle Scholar
Beaudoin, N, Huyghe, D, Bellahsen, N, Lacombe, O, Emmanuel, L, Mouthereau, F and Ouanhnon, L (2015) Fluid systems and fracture development during syn-depositional fold growth: an example from the Pico del Aguila anticline, Sierras Exteriores, southern Pyrenees, Spain. Journal of Structural Geology 70, 23–38.CrossRefGoogle Scholar
Beaudoin, N, Koehn, D, Lacombe, O, Lecouty, A, Billi, A, Aharonov, E and Parlangeau, C (2016) Fingerprinting stress: stylolite and calcite twinning paleopiezometry revealing the complexity of progressive stress patterns during folding: the case of the Monte Nero anticline in the Apennines, Italy. Tectonics 35, 1687–712.CrossRefGoogle Scholar
Beaudoin, NE, Labeur, A, Lacombe, O, Koehn, D, Billi, A, Hoareau, G, Boyce, A, John, CM, Marchegiano, M, Roberts, NM, Millar, IL, Claverie, F, Pecheyran, C and Callot, JP (2020c) Regional-scale paleofluid system across the Tuscan Nappe-Umbria-Marche Apennine Ridge (northern Apennines) as revealed by mesostructural and isotopic analyses of stylolite-vein networks. Solid Earth 11, 1617–41.CrossRefGoogle Scholar
Beaudoin, N, Lacombe, O, David, ME and Koehn, D (2020a) Does stress transmission in forelands depend on structural style? Distinctive stress magnitudes during Sevier thin-skinned and Laramide thick-skinned layer-parallel shortening in the Bighorn Basin (USA) revealed by stylolite and calcite twinning paleopiezometry. Terra Nova 32, 225–33.CrossRefGoogle Scholar
Beaudoin, N, Lacombe, O, Koehn, D, David, ME, Farrell, N and Healy, D (2020b) Vertical stress history and paleoburial in foreland basins unravelled by stylolite roughness paleopiezometry: insights from bedding-parallel stylolites in the Bighorn Basin, Wyoming, USA. Journal of Structural Geology 136, 104061.CrossRefGoogle Scholar
Beaudoin, N, Lacombe, O, Roberts, NMW and Koehn, D (2018) U-Pb dating of calcite veins reveals complex stress evolution and thrust sequence in the Bighorn Basin, Wyoming, USA. Geology 46, 1015–8.CrossRefGoogle Scholar
Beaudoin, N, Lacombe, O, Roberts, NMW and Koehn, D (2019a) U-Pb dating of calcite veins reveals complex stress evolution and thrust sequence in the Bighorn Basin, Wyoming, USA: REPLY. Geology 47, e481.CrossRefGoogle Scholar
Becker, JS (2002) State-of-the-art and progress in precise and accurate isotope ratio measurements by ICP-MS and LA-ICP-MS. Journal of Analytical Atomic Spectrometry 17, 1172–85.CrossRefGoogle Scholar
Bellahsen, N, Fiore, PE and Pollard, DD (2006a) From spatial variation of fracture patterns to fold kinematics: a geomechanical approach. Geophysical Research Letters 33, 1–4.CrossRefGoogle Scholar
Bellahsen, N, Fiore, P and Pollard, DD (2006b) The role of fractures in the structural interpretation of Sheep Mountain Anticline, Wyoming. Journal of Structural Geology 28, 850–67.CrossRefGoogle Scholar
Bense, VF, Gleeson, T, Loveless, SE, Bour, O and Scibek, J (2013) Fault zone hydrogeology. Earth-Science Reviews 127, 171–92.CrossRefGoogle Scholar
Bergbauer, S and Pollard, DD (2004) A new conceptual fold-fracture model including prefolding joints, based on the Emigrant Gap anticline, Wyoming. Bulletin of the Geological Society of America 116, 294–307.CrossRefGoogle Scholar
Bergman, SC, Huntington, KW and Crider, JG (2013) Tracing paleofluid sources using clumped isotope thermometry of diagenetic cements along the Moab Fault, Utah. American Journal of Science 313, 490–515.CrossRefGoogle Scholar
Berio, LR, Mittempergher, S, Storti, F, Bernasconi, SM, Cipriani, A, Lugli, F and Balsamo, F (2022) Open-closed-open paleofluid system conditions recorded in the tectonic vein networks of the Parmelan anticline (Bornes Massif, France). Journal of the Geological Society 179 (5), 2021–117. https://doi.org/10.1144/jgs2021-117.CrossRefGoogle Scholar
Bernasconi, SM, Daëron, M, Bergmann, KD, Bonifacie, M, Meckler, AN, Affek, HP, Anderson, N, Bajnai, D, Barkan, E, Beverly, E, Blamart, D, Burgener, L, Calmels, D, Chaduteau, C, Clog, M, Davidheiser-Kroll, B, Davies, A, Dux, F, Eiler, J, Elliott, B, Fetrow, AC, Fiebig, J, Goldberg, S, Hermoso, M, Huntington, KW, Hyland, E, Ingalls, M, Jaggi, M, John, CM, Jost, AB, Katz, S, Kelson, J, Kluge, T, Kocken, IJ, Laskar, A, Leutert, TJ, Liang, D, Lucarelli, J, Mackey, TJ, Mangenot, X, Meinicke, N, Modestou, SE, Müller, IA, Murray, S, Neary, A, Packard, N, Passey, BH, Pelletier, E, Petersen, S, Piasecki, A, Schauer, A, Snell, KE, Swart, PK, Tripati, A, Upadhyay, D, Vennemann, T, Winkelstern, I, Yarian, D, Yoshida, N, Zhang, N and Ziegler, M (2021) InterCarb: a community effort to improve interlaboratory standardization of the carbonate clumped isotope thermometer using carbonate standards. Geochemistry, Geophysics, Geosystems 22, e2020GC009588.CrossRefGoogle ScholarPubMed
Bernasconi, SM, Müller, IA, Bergmann, KD, Breitenbach, SFM, Fernandez, A, Hodell, DA, Jaggi, M, Meckler, AN, Millan, I and Ziegler, M (2018) Reducing uncertainties in carbonate clumped isotope analysis through consistent carbonate-based standardization. Geochemistry, Geophysics, Geosystems 19, 2895–914.CrossRefGoogle ScholarPubMed
Bilau, A, Bienveignant, D, Rolland, Y, Schwartz, S, Godeau, N, Guihou, A, Deschamps, P, Mangenot, X, Brigaud, B, Boschetti, L and Dumont, T (2022) The Tertiary structuration of the Western Subalpine foreland deciphered by calcite-filled faults and veins. Earth-Science Reviews 236, 104270.CrossRefGoogle Scholar
Bjørlykke, K (1994) Fluid-flow processes and diagenesis in sedimentary basins. In Geofluids: Origin, Migration and Evolution of Fluids in Sedimentary Basins (ed. Farrell, J.), pp. 127–40. Geological Society of London, Special Publication no. 78.Google Scholar
Bjørlykke, K (2015) Subsurface water and fluid flow in sedimentary basins. In Petroleum Geoscience: From Sedimentary Environments to Rock Physics, 2nd edn., pp. 279–300. Berlin: Springer.CrossRefGoogle Scholar
Blamey, NJF (2012) Composition and evolution of crustal, geothermal and hydrothermal fluids interpreted using quantitative fluid inclusion gas analysis. Journal of Geochemical Exploration 116–117, 17–27.CrossRefGoogle Scholar
Bodnar, RJ (2003) Reequilibration of fluid inclusions. In Fluid Inclusions: Analysis and Interpretation (eds Samson, I, Anderson, A and Marshall, D), pp. 213–30. Vancouver, Canada: Mineralogical Association of Canada Short Course 32.Google Scholar
Boggs, S and Krinsley, D (2006) Application of Cathodoluminescence Imaging to the Study of Sedimentary Rocks. Cambridge: Cambridge University Press.CrossRefGoogle Scholar
Böhlke, JK and Irwin, JJ (1992) Laser microprobe analyses of noble gas isotopes and halogens in fluid inclusions: analyses of microstandards and synthetic inclusions in quartz. Geochimica et Cosmochimica Acta 56, 187–201.CrossRefGoogle Scholar
Bonifacie, M, Calmels, D, Eiler, JM, Horita, J, Chaduteau, C, Vasconcelos, C, Agrinier, P, Katz, A, Passey, BH, Ferry, JM and Bourrand, JJ (2017) Calibration of the dolomite clumped isotope thermometer from 25 to 350 °C, and implications for a universal calibration for all (Ca, Mg, Fe) CO3 carbonates. Geochimica et Cosmochimica Acta 200, 255–79.CrossRefGoogle Scholar
Bons, PD, Elburg, MA and Gomez-Rivas, E (2012) A review of the formation of tectonic veins and their microstructures. Journal of Structural Geology 43, 33–62.CrossRefGoogle Scholar
Bottinga, Y (1969) Calculated fractionation factors for carbon and hydrogen isotope exchange in the system calcite-carbon dioxide-graphite-methane-hydrogen-water vapor. Geochimica et Cosmochimica Acta 33, 49–64.CrossRefGoogle Scholar
Bottinga, Y and Craig, H (1968) Oxygen isotope fractionation between CO2 and water, and the isotopic composition of marine atmospheric CO2 . Earth and Planetary Science Letters 5, 285–95.CrossRefGoogle Scholar
Bourdet, J, Pironon, J, Levresse, G and Tritlla, J (2008) Petroleum type determination through homogenization temperature and vapour volume fraction measurements in fluid inclusions. Geofluids 8, 46–59.CrossRefGoogle Scholar
Bradbury, HJ and Woodwell, GR (1987) Ancient fluid flow within foreland terrains. In Petroleum Geology of the Continental Shelf of Northwest Europe: Oil and Source Rocks of the North Sea (eds LV Illing and GD Hobson), pp. 87–102. Geological Society of London, Special Publication no. 34.CrossRefGoogle Scholar
Braithwaite, CJR (1989) Stylolites as open fluid conduits. Marine and Petroleum Geology 6, 93–96.Google Scholar
Brannon, JC, Cole, SC, Podosek, FA, Ragan, VM, Coveney, RM, Wallace, MW and Bradley, AJ (1996) Th-Pb and U-Pb dating of ore-stage calcite and Paleozoic fluid flow. Science 271, 491–3.CrossRefGoogle Scholar
Breesch, L, Swennen, R, Dewever, B, Roure, F and Vincent, B (2011) Diagenesis and fluid system evolution in the northern Oman Mountains, United Arab Emirates: implications for petroleum exploration. GeoArabia 16, 111–48.CrossRefGoogle Scholar
Breesch, L, Swennen, R and Vincent, B (2006) Dolomite formation in breccias at the Musandam Platform border, Northern Oman Mountains, United Arab Emirates. Journal of Geochemical Exploration 89, 19–22.CrossRefGoogle Scholar
Breesch, L, Swennen, R and Vincent, B (2009) Fluid flow reconstruction in hanging and footwall carbonates: compartmentalization by Cenozoic reverse faulting in the Northern Oman Mountains (UAE). Marine and Petroleum Geology 26, 113–28.CrossRefGoogle Scholar
Breesch, L, Swennen, R, Vincent, B, Ellison, R and Dewever, B (2010) Dolomite cementation and recrystallisation of sedimentary breccias along the Musandam Platform margin (United Arab Emirates). Journal of Geochemical Exploration 106, 34–43.CrossRefGoogle Scholar
Bruna, PO, Lavenu, APC, Matonti, C and Bertotti, G (2019) Are stylolites fluid-flow efficient features? Journal of Structural Geology 125, 270–7.CrossRefGoogle Scholar
Caine, JS, Evans, JP and Forster, CB (1996) Fault zone architecture and permeability structure. Geology 24, 1025–8.2.3.CO;2>CrossRefGoogle Scholar
Caja, MA, Permanyer, A, Marfil, R, Al-Aasm, IS and Martín-Crespo, T (2006) Fluid flow record from fracture-fill calcite in the Eocene limestones from the South-Pyrenean Basin (NE Spain) and its relationship to oil shows. Journal of Geochemical Exploration 89, 27–32.CrossRefGoogle Scholar
Calamita, F, Satolli, S, Scisciani, V, Esestime, P and Pace, P (2011) Contrasting styles of fault reactivation in curved orogenic belts: examples from the central Apennines (Italy). Bulletin of the Geological Society of America 123, 1097–111.CrossRefGoogle Scholar
Callot, JP, Breesch, L, Guilhaumou, N, Roure, F, Swennen, R and Vilasi, N (2010b) Paleo-fluids characterisation and fluid flow modelling along a regional transect in Northern United Arab Emirates (UAE). Arabian Journal of Geosciences 3, 413–37.CrossRefGoogle Scholar
Callot, JP, Robion, P, Sassi, W, Guiton, MLE, Faure, JL, Daniel, JM, Mengus, JM and Schmitz, J (2010a) Magnetic characterisation of folded aeolian sandstones: interpretation of magnetic fabrics in diamagnetic rocks. Tectonophysics 495, 230–45.CrossRefGoogle Scholar
Callot, JP, Sassi, W, Roure, F, Hill, K, Wilson, N and Divies, R (2017) Pressure and Basin modeling in Foothill belts: a study of the Kutubu area, Papua New Guinea Fold and Thrust Belt. AAPG Memoir 114, 165–89.Google Scholar
Callot, JP, Trocmé, V, Letouzey, J, Albouy, E, Jahani, S and Sherkati, S (2012) Pre-existing salt structures and the folding of the Zagros Mountains. In Salt Tectonics, Sediments and Prospectivity (ed. SG Archer), pp. 545–61. Geological Society of London, Special Publication no. 363.CrossRefGoogle Scholar
Capozzi, R and Picotti, V (2002) Fluid migration and origin of a mud volcano in the Northern Apennines (Italy): the role of deeply rooted normal faults. Terra Nova 14, 363–70.CrossRefGoogle Scholar
Caricchi, C, Aldega, L and Corrado, S (2014) Reconstruction of maximum burial along the Northern Apennines thrust wedge (Italy) by indicators of thermal exposure and modeling. Bulletin of the Geological Society of America 127, 428–42.CrossRefGoogle Scholar
Cathles, LM (1981) Fluid flow and genesis of hydrothermal ore deposits. In Economic Geology, Seventy-fifth Anniversary Volume (1905–1980) (eds. Brian J Skinner), pp. 424–57. El Paso, USA: The Economic Geology Publishing Company.Google Scholar
Caumon, M-C, Dubessy, J, Robert, P and Tarantola, A (2014) Fused-silica capillary capsules (FSCCs) as reference synthetic aqueous fluid inclusions to determine chlorinity by Raman spectroscopy. European Journal of Mineralogy 25, 755–63.CrossRefGoogle Scholar
Cello, G, Invernizzi, C, Mazzoli, S and Tondi, E (2001) Fault properties and fluid flow patterns from Quaternary faults in the Apennines, Italy. Tectonophysics 336, 63–78.CrossRefGoogle Scholar
Centrella, S, Beaudoin, NE, Derluyn, H, Motte, G, Hoareau, G, Lanari, P, Piccoli, F, Pecheyran, C and Callot, JP (2021) Micro-scale chemical and physical patterns in an interface of hydrothermal dolomitization reveals the governing transport mechanisms in nature: case of the Layens anticline, Pyrenees, France. Sedimentology 68, 834–54.CrossRefGoogle Scholar
Centrella, S, Beaudoin, NE, Koehn, D, Motte, G, Hoareau, G and Callot, JP (2022) How fluid-mediated rock transformations can mimic hydro-fracturing patterns in hydrothermal dolomite. Marine and Petroleum Geology 140, 105657.CrossRefGoogle Scholar
Centrella, S, Putnis, A, Lanari, P and Austrheim, H (2018) Textural and chemical evolution of pyroxene during hydration and deformation: a consequence of retrograde metamorphism. Lithos 296–299, 245–64.CrossRefGoogle Scholar
Chacko, T and Deines, P (2008) Theoretical calculation of oxygen isotope fractionation factors in carbonate systems. Geochimica et Cosmochimica Acta 72, 3642–60.CrossRefGoogle Scholar
Chen, S, Ryb, U, Piasecki, AM, Lloyd, MK, Baker, MB and Eiler, JM (2019) Mechanism of solid-state clumped isotope reordering in carbonate minerals from aragonite heating experiments. Geochimica et Cosmochimica Acta 258, 156–73.CrossRefGoogle Scholar
Chi, G, Diamond, LW, Lu, H, Lai, J and Chu, H (2020) Common problems and pitfalls in fluid inclusion study: a review and discussion. Minerals 2021, 7–11. https://doi.org/10.3390/MIN11010007.CrossRefGoogle Scholar
Choukroune, P (1992) Tectonic evolution of the Pyrenees. Annual Review of Earth and Planetary Sciences 20, 143.CrossRefGoogle Scholar
Clauer, N (2013) The K-Ar and 40Ar/39Ar methods revisited for dating fine-grained K-bearing clay minerals. Chemical Geology 354, 163–85.CrossRefGoogle Scholar
Cobbold, PR, Zanella, A, Rodrigues, N and Løseth, H (2013) Bedding-parallel fibrous veins (beef and cone-in-cone): worldwide occurrence and possible significance in terms of fluid overpressure, hydrocarbon generation and mineralization. Marine and Petroleum Geology 43, 1–20.CrossRefGoogle Scholar
Cooley, MA, Price, RA, Kyser, TK and Dixon, JM (2011) Stable-isotope geochemistry of syntectonic veins in Paleozoic carbonate rocks in the Livingstone Range anticlinorium and their significance to the thermal and fluid evolution of the southern Canadian foreland thrust and fold belt. AAPG Bulletin 95, 1851–82.CrossRefGoogle Scholar
Coppola, M, Correale, A, Barberio, MD, Billi, A, Cavallo, A, Fondriest, M, Nazzari, M, Paonita, A, Romano, C, Stagno, V, Viti, C and Vona, JM (2021) Meso- to nano-scale evidence of fluid-assisted co-seismic slip along the normal Mt. Morrone Fault, Italy: implications for earthquake hydrogeochemical precursors. Earth and Planetary Science Letters 568, 117010.CrossRefGoogle Scholar
Craddock, JP and Relle, M (2003) Fold axis-parallel rotation within the Laramide Derby Dome Fold, Wind River Basin, Wyoming, USA. Journal of Structural Geology 25, 1959–72.CrossRefGoogle Scholar
Craddock, JP and van der Pluijm, BA (1989) Late Paleozoic deformation of the cratonic carbonate cover of eastern North America. Geology 17, 416–9.2.3.CO;2>CrossRefGoogle Scholar
Craddock, JP and van der Pluijm, BA (1999) Sevier-Laramide deformation of the continental interior from calcite twinning analysis, west-central North America. Tectonophysics 305, 275–86.CrossRefGoogle Scholar
Craig, H (1957) Isotopic standards for carbon and oxygen and correction factors for mass-spectrometric analysis of carbon dioxide. Geochimica et Cosmochimica Acta 12, 133–49.CrossRefGoogle Scholar
Craig, H (1961) Standard for reporting concentrations of deuterium and oxygen-18 in natural waters. Science 133, 1833–4.CrossRefGoogle ScholarPubMed
Crognier, N, Hoareau, G, Aubourg, C, Dubois, M, Lacroix, B, Branellec, M, Callot, JP and Vennemann, T (2018) Syn-orogenic fluid flow in the Jaca basin (south Pyrenean fold and thrust belt) from fracture and vein analyses. Basin Research 30, 187–216.CrossRefGoogle Scholar
Cruset, D, Cantarero, I, Travé, A, Vergés, J and John, CM (2016) Crestal graben fluid evolution during growth of the Puig-Reig anticline (South Pyrenean fold and thrust belt). Journal of Geodynamics 101, 30–50.CrossRefGoogle Scholar
Cruset, D, Cantarero, I, Vergés, J, John, CM, Muñoz-López, D and Travé, A (2018) Changes in fluid regime in syn-orogenic sediments during the growth of the south Pyrenean fold and thrust belt. Global and Planetary Change 171, 207–24.CrossRefGoogle Scholar
Cruset, D, Vergés, J, Benedicto, A, Gomez-Rivas, E, Cantarero, I, John, CM and Travé, A (2021) Multiple fluid flow events from salt-related rifting to basin inversion (Upper Pedraforca thrust sheet, SE Pyrenees). Basin Research 33, 3102–36.CrossRefGoogle Scholar
Curtis, CD (1987) Inorganic geochemistry and petroleum exploration. In Advances in Petroleum Geochemistry (eds Brooks, J and Welte, D), pp. 91–141. London: Academic Press.Google Scholar
Curzi, M, Aldega, L, Bernasconi, SM, Berra, F, Billi, A, Boschi, C, Franchini, S, van der Lelij, R, Viola, G and Carminati, E (2020) Architecture and evolution of an extensionally-inverted thrust (Mt. Tancia Thrust, Central Apennines): geological, structural, geochemical, and K–Ar geochronological constraints. Journal of Structural Geology 136, 104059.CrossRefGoogle Scholar
Curzi, M, Bernasconi, SM, Billi, A, Boschi, C, Aldega, L, Franchini, S, Albert, R, Gerdes, A, Barberio, MD and Carminati, E (2021) U–Pb age of the 2016 Amatrice earthquake causative fault (Mt. Gorzano, Italy) and paleo-fluid circulation during seismic cycles inferred from inter-and co-seismic calcite. Tectonophysics 819, 229076.CrossRefGoogle Scholar
Daëron, M (2021) Full propagation of analytical uncertainties in Δ47 measurements. Geochemistry, Geophysics, Geosystems 22, e2020GC009592.CrossRefGoogle Scholar
D’Amore, F and Panichi, C (1980) Evaluation of deep temperatures of hydrothermal systems by a new gas geothermometer. Geochimica et Cosmochimica Acta 44, 549–56.CrossRefGoogle Scholar
Dassié, EP, Genty, D, Noret, A, Mangenot, X, Massault, M, Lebas, N, Duhamel, M, Bonifacie, M, Gasparrini, M, Minster, B and Michelot, JL (2018) A newly designed analytical line to examine fluid inclusion isotopic compositions in a variety of carbonate samples. Geochemistry, Geophysics, Geosystems 19, 1107–22.CrossRefGoogle Scholar
Davies, GR and Smith, LB (2006) Structurally controlled hydrothermal dolomite reservoir facies: an overview. American Association of Petroleum Geologists Bulletin 90, 1641–90.CrossRefGoogle Scholar
Davis, DW, Lowenstein, TK and Spencer, RJ (1990) Melting behavior of fluid inclusions in laboratory-grown halite crystals in the systems NaCl-H2O, NaCl-KCl-H2O, NaCl-MgCl2-H2O, and NaCl-CaCl2-H2O. Geochimica et Cosmochimica Acta 54, 591–601 CrossRefGoogle Scholar
de Graaf, S, Nooitgedacht, CW, Goff, JLE, van der Lubbe, JHJL, Vonhof, HB and Reijmer, JJG (2019) Fluid-flow evolution in the Albanide fold-thrust belt: insights from hydrogen and oxygen isotope ratios of fluid inclusions. AAPG Bulletin 103, 2421–45.CrossRefGoogle Scholar
del Sole, L, Antonellini, M, Soliva, R, Ballas, G, Balsamo, F and Viola, G (2020) Structural control on fluid flow and shallow diagenesis: insights from calcite cementation along deformation bands in porous sandstones. Solid Earth 11, 2169–195.CrossRefGoogle Scholar
DeCelles, PG (2004). Late Jurassic to Eocene evolution of the Cordilleran thrust belt and foreland basin system, western USA. American Journal of Science 304, 105–68.CrossRefGoogle Scholar
Dellinger, M, Gaillardet, J, Bouchez, J, Calmels, D, Louvat, P, Dosseto, A, Gorge, C, Alanoca, L and Maurice, L (2015) Riverine Li isotope fractionation in the Amazon River basin controlled by the weathering regimes. Geochimica et Cosmochimica Acta 164, 71–93.CrossRefGoogle Scholar
Deloule, E and Turcotte, DL (1989) The flow of hot brines in cracks and the formation of ore deposits. Economic Geology 84, 2217–25.CrossRefGoogle Scholar
Dielforder, A, Villa, IM, Berger, A and Herwegh, M (2022) Tracing wedge-internal deformation by means of strontium isotope systematics of vein carbonates. Geological Magazine. https://doi.org/10.1017/ S0016756821001357 CrossRefGoogle Scholar
Dielforder, A, Vollstaedt, H, Vennemann, T, Berger, A and Herwegh, M (2015) Linking megathrust earthquakes to brittle deformation in a fossil accretionary complex. Nature Communications 6, 7504.CrossRefGoogle Scholar
Dreybrodt, W and Deininger, M (2014) The impact of evaporation to the isotope composition of DIC in calcite precipitating water films in equilibrium and kinetic fractionation models. Geochimica et Cosmochimica Acta 125, 433–9.CrossRefGoogle Scholar
Dromgoole, EL.and Walter, LM (1990) Iron and manganese incorporation into calcite: effects of growth kinetics, temperature and solution chemistry. Chemical Geology 81, 311–36.CrossRefGoogle Scholar
Drost, K, Chew, D, Petrus, JA, Scholze, F, Woodhead, J D, Schneider, JW and Harper, DA (2018) An image mapping approach to U-Pb LA-ICP-MS carbonate dating and applications to direct dating of carbonate sedimentation. Geochemistry, Geophysics, Geosystems 19, 4631–48.CrossRefGoogle Scholar
Eichhubl, P, Taylor, WL, Pollard, DD and Aydin, A (2004) Paleo-fluid flow and deformation in the Aztec Sandstone at the Valley of Fire, Nevada: evidence for the coupling of hydrogeologic, diagenetic, and tectonic processes. GSA Bulletin 116, 1120–36.CrossRefGoogle Scholar
Eiler, JM and Schauble, E (2004) 18O13C16O in Earth’s atmosphere. Geochimica et Cosmochimica Acta 68, 4767–77.CrossRefGoogle Scholar
Elter, P, Grasso, M, Parotto, M and Vezzani, L (2008) Structural setting of the Apennine-Maghrebian thrust belt. Episodes 26, 205–11.CrossRefGoogle Scholar
Emery, D and Robinson, A (1993) Inorganic Geochemistry: Applications to Petroleum Geology, 255 pp. Oxford, UK: Blackwell Scientific Publications.CrossRefGoogle Scholar
Engel, J, Maas, R, Woodhead, J, Tympel, J and Greig, A (2020) A single-column extraction chemistry for isotope dilution U-Pb dating of carbonate. Chemical Geology 531, 119311.CrossRefGoogle Scholar
English, JM, Johnston, ST and Wang, K (2003). Thermal modelling of the Laramide orogeny: testing the flat-slab subduction hypothesis. Earth and Planetary Science Letters 214, 619–32.CrossRefGoogle Scholar
Epstein, S, Buchsbaum, R, Lowenstam, HA and Urey, HC (1953) Revised carbonate-water isotopic temperature scale. GSA Bulletin 64, 1315–26.CrossRefGoogle Scholar
Erslev, EA (1986) Basement balancing of Rocky Mountain foreland uplifts (USA). Geology 14, 259–62.2.0.CO;2>CrossRefGoogle Scholar
Evans, MA (2010) Temporal and spatial changes in deformation conditions during the formation of the Central Appalachian fold-and-thrust belt: evidence from joints, vein mineral paragenesis, and fluid inclusions. In From Rodinia to Pangea: The Lithotectonic Record of the Appalachian Region (ed. Tollo, RP), pp. 417–518: Boulder, Colorado: Geological Society of America. GSA Memoir.Google Scholar
Evans, MA and Battle, DA (1999) Fluid inclusion and stable isotope analyses of veins from the central Appalachian Valley and Ridge province: implications for regional synorogenic hydrologic structure and fluid migration. GSA Bulletin 111, 1841–60.2.3.CO;2>CrossRefGoogle Scholar
Evans, MA, Bebout, GE and Brown, CH (2012) Changing fluid conditions during folding: an example from the central Appalachians. Tectonophysics 576–577, 99–115.CrossRefGoogle Scholar
Evans, MA and Fischer, MP (2012) On the distribution of fluids in folds: a review of controlling factors and processes. Journal of Structural Geology 44, 2–24.CrossRefGoogle Scholar
Evans, MA and Hobbs, GC (2003) Fate of ‘warm’ migrating fluids in the central Appalachians during the Late Paleozoic Alleghanian orogeny. Journal of Geochemical Exploration 78–79, 327–31.CrossRefGoogle Scholar
Fantle, MS and Higgins, J (2014) The effects of diagenesis and dolomitization on Ca and Mg isotopes in marine platform carbonates: implications for the geochemical cycles of Ca and Mg. Geochimica et Cosmochimica Acta 142, 458–81.CrossRefGoogle Scholar
Faulkner, DR, Jackson, CAL, Lunn, RJ, Schlische, RW, Shipton, ZK, Wibberley, CAJ and Withjack, MO (2010) A review of recent developments concerning the structure, mechanics and fluid flow properties of fault zones. Journal of Structural Geology 32, 1557–75.CrossRefGoogle Scholar
Ferket, H, Guilhaumou, N, Roure, F and Swennen, R (2011) Insights from fluid inclusions, thermal and PVT modeling for paleo-burial and thermal reconstruction of the Córdoba petroleum system (NE Mexico). Marine and Petroleum Geology 28, 936–58.CrossRefGoogle Scholar
Ferket, H, Roure, F, Swennen, R and Ortuño, S (2000) Fluid migration placed into the deformation history of fold-and-thrust belts: an example from the Veracruz basin (Mexico). Journal of Geochemical Exploration 69–70, 275–9.CrossRefGoogle Scholar
Ferket, H, Swennen, R, Ortuño, S and Roure, F (2003) Reconstruction of the fluid flow history during Laramide forelandfold and thrust belt development in eastern Mexico: cathodoluminescence and δ18O-δ13C isotope trends of calcite-cemented fractures. Journal of Geochemical Exploration 78–79, 163–7.CrossRefGoogle Scholar
Ferket, H, Swennen, R, Ortuño Arzate, S and Roure, F (2006) Fluid flow evolution in petroleum reservoirs with a complex diagenetic history: an example from Veracruz, Mexico. Journal of Geochemical Exploration 89, 108–11.CrossRefGoogle Scholar
Fischer, MP, Higuera-Díaz, IC, Evans, MA, Perry, EC and Lefticariu, L (2009) Fracture-controlled paleohydrology in a map-scale detachment fold: insights from the analysis of fluid inclusions in calcite and quartz veins. Journal of Structural Geology 31, 1490–510.CrossRefGoogle Scholar
Fischer, MP and Jackson, PB (1999) Stratigraphic controls on deformation patterns in fault-related folds: a detachment fold example from the Sierra Madre Oriental, northeast Mexico. Journal of Structural Geology 21, 613–33.CrossRefGoogle Scholar
Fitz-Diaz, E, Hudleston, P, Siebenaller, L, Kirschner, D, Camprubí, A, Tolson, G and Puig, TP (2011a) Insights into fluid flow and water-rock interaction during deformation of carbonate sequences in the Mexican fold-thrust belt. Journal of Structural Geology 33, 1237–53.CrossRefGoogle Scholar
Fitz-Diaz, E, Hudleston, P and Tolson, G (2011b) Comparison of tectonic styles in the Mexican and Canadian Rocky Mountain Fold-Thrust Belt. In Kinematic Evolution and Structural Styles of Fold-and-Thrust Belts (eds Poblet, J and Lisle, RJ), pp.149–67. Geological Society of London, Special Publication no. 349.Google Scholar
Fossen, H, Schultz, RA. Shipton, ZK and Mair, K (2007) Deformation bands in sandstone: a review. Journal of the Geological Society 164, 755–69.CrossRefGoogle Scholar
Gabellone, T, Gasparrini, M, Iannace, A, Invernizzi, C, Mazzoli, S and D’Antonio, M (2013) Fluid channeling along thrust zones: the Lagonegro case history, southern Apennines, Italy. Geofluids 13, 140–58.CrossRefGoogle Scholar
Gao, J, He, S, Zhao, JX, He, Z, Wu, C, Feng, Y, Nguyen, AD, Zhou, J and Yi, Z (2020) Sm-Nd isochron dating and geochemical (rare earth elements, 87Sr/86Sr, δ18O, δ13C) characterization of calcite veins in the Jiaoshiba shale gas field, China: implications for the mechanisms of vein formation in shale gas systems. GSA Bulletin 132, 1722–40.CrossRefGoogle Scholar
Ge, S and Garven, G (1994) A theoretical model for thrust-induced deep groundwater expulsion with application to the Canadian Rocky Mountains. Journal of Geophysical Research 99, 13851–868.CrossRefGoogle Scholar
Ghisetti, F, Kirschner, DL, Vezzani, L and Agosta, F (2001) Stable isotope evidence for contrasting paleofluid circulation in thrust faults and normal faults of the central Apennines, Italy. Journal of Geophysical Research: Solid Earth 106, 8811–25.CrossRefGoogle Scholar
Ghisetti, F and Vezzani, L (2000) Detachments and normal faulting in the Marche fold-and-thrust belt (central Apennines, Italy): inferences on fluid migration paths. Journal of Geodynamics 29, 345–69.CrossRefGoogle Scholar
Ghosh, P, Adkins, J, Affek, H, Balta, B, Guo, W, Schauble, EA, Schrag, D and Eiler, JM (2006) 13C-18O bonds in carbonate minerals: a new kind of paleothermometer. Geochimica et Cosmochimica Acta 70, 1439–56.CrossRefGoogle Scholar
Giggenbach, WF (1996) Chemical composition cf volcanic gases. In Monitoring and Mitigation of Volcano Hazards, (eds Scarpa/Tilling), pp. 221–56. Germany: Springer-Verlag Berlin.Google Scholar
Goldstein, RH (1986) Reequilibration of fluid inclusions in low-temperature calcium-carbonate cement. Geology 14, 792–5.2.0.CO;2>CrossRefGoogle Scholar
Goldstein, RH and Reynolds, TJ (1994) Systematics of Fluid Inclusions in Diagenetic Minerals. SEPM Short Course 31, 213 pp.CrossRefGoogle Scholar
Gomez-Rivas, E, Corbella, M, Martín-Martín, JD, Stafford, SL, Teixell, A, Bons, PD, Griera, A and Cardellach, E (2014) Reactivity of dolomitizing fluids and Mg source evaluation of fault-controlled dolomitization at the Benicàssim outcrop analogue (Maestrat basin, E Spain). Marine and Petroleum Geology 55, 26–42.CrossRefGoogle Scholar
Gonzalez, E, Ferket, H, Callot, J-P, Guillhaumou, N, Ortuno, S and Roure, F (2012) Paleoburial, hydrocarbon generation, and migration in the Córdoba Platform and Veracruz Basin: insights from fluid inclusion studies and two-dimensional (2D) basin modeling. In Analyzing the Thermal History of Sedimentary Basins: Methods and Case Studies (ND Naeser and TH McCulloh), pp. 167–86. Tulsa, Oklahoma: SEPM Special Publication.Google Scholar
Gratier, JP, Frery, E, Deschamps, P, Røyne, A, Renard, F, Dysthe, D, Ellouz-Zimmerman, N and Hamelin, B (2012) How travertine veins grow from top to bottom and lift the rocks above them: the effect of crystallization force. Geology 40, 1015–18.CrossRefGoogle Scholar
Graustein, WC (1989) 87Sr/86Sr ratios measure the sources and flow of strontium in terrestrial ecosystems. In Stable Isotopes in Ecological Research. Ecological Studies (Analysis and Synthesis) (eds Rundel, PW, Ehleringer, JR and Nagy, KA), pp. 491–512. New York: Springer.CrossRefGoogle Scholar
Groshong, RH, Kronenberg, A, Couzens-Schultz, BA and Newman, J (2014) Fluids and structures in fold and thrust belts with recognition of the work of David Wiltschko. Journal of Structural Geology 69, 281–3.CrossRefGoogle Scholar
Guillaume, D, Teinturier, S, Dubessy, J and Pironon, J (2003) Calibration of methane analysis by Raman spectroscopy in H2O–NaCl–CH4 fluid inclusions. Chemical Geology 194, 41–9.CrossRefGoogle Scholar
Guiton, MLE, Leroy, YM and Sassi, W (2003) Activation of diffuse discontinuities and folding of sedimentary layers. Journal of Geophysical Research: Solid Earth 108, 1–20.CrossRefGoogle Scholar
Gussone, N, Ahm, ASC, Lau, KV and Bradbury, HJ (2020) Calcium isotopes in deep time: potential and limitations. Chemical Geology 544, 119601.CrossRefGoogle Scholar
Haines, S, Lynch, E, Mulch, A, Valley, JW and van der Pluijm, B (2016) Meteoric fluid infiltration in crustal-scale normal fault systems as indicated by δ18O and δ2H geochemistry and 40Ar/39Ar dating of neoformed clays in brittle fault rocks. Lithosphere 8, 587–600.CrossRefGoogle Scholar
Haines, SH and van der Pluijm, BA (2008) Clay quantification and Ar–Ar dating of synthetic and natural gouge: application to the Miocene Sierra Mazatán detachment fault, Sonora, Mexico. Journal of Structural Geology 30, 525–38.CrossRefGoogle Scholar
Hairuo Qing and Mountjoy, EW (1994) Formation of coarsely crystalline, hydrothermal dolomite reservoirs in the Presqu’ile Barrier, Western Canada Sedimentary Basin. AAPG Bulletin 78, 55–77.Google Scholar
Hanks, CL, Parris, TM and Wallace, WK (2006) Fracture paragenesis and microthermometry in Lisburne Group detachment folds: implications for the thermal and structural evolution of the northeastern Brooks Range, Alaska. AAPG Bulletin 90, 1–20.CrossRefGoogle Scholar
Heap, M, Reuschlé, T, Baud, P, Renard, F and Iezzi, G (2018) The permeability of stylolite-bearing limestone. Journal of Structural Geology 116, 81–93.CrossRefGoogle Scholar
Heinze, T, Hamidi, S and Galvan, B. (2017). A dynamic heat transfer coefficient between fractured rock and flowing fluid. Geothermics 65, 10–16.CrossRefGoogle Scholar
Henderson, IHC and McCaig, AM (1996) Fluid pressure and salinity variations in shear zone-related veins, central Pyrenees, France: implications for the fault-valve model. Tectonophysics 262, 321–48.CrossRefGoogle Scholar
Henley, R, Truesdell, A, Barton, P and Whitney, J (1984) Fluid-mineral equilibria in hydrothermal systems. In Reviews in Economic Geology 1 (eds Henley, Truesdell and Barton, Jr). Littleton, USA: Society of Economic Geologists.CrossRefGoogle Scholar
Hilgers, C, Dilg-Gruschinski, K and Urai, JL (2004) Microstructural evolution of syntaxial veins formed by advective flow. Geology 32, 261–4.CrossRefGoogle Scholar
Hilgers, C, Kirschner, DL, Breton, JP and Urai, JL (2006) Fracture sealing and fluid overpressures in limestones of the Jabal Akhdar dome, Oman Mountains. Geofluids 6, 168–84.CrossRefGoogle Scholar
Hilgers, C and Urai, JL (2002a) Experimental study of syntaxial vein growth during lateral fluid flow in transmitted light: first results. Journal of Structural Geology 24, 1029–43.CrossRefGoogle Scholar
Hilgers, C and Urai, JL (2002b) Microstructural observations on natural syntectonic fibrous veins: implications for the growth process. Tectonophysics 352, 257–74.CrossRefGoogle Scholar
Hnat, JS and van der Pluijm, BA (2014) Fault gouge dating in the Southern Appalachians, USA. GSA Bulletin 126, 639–51.CrossRefGoogle Scholar
Hoareau, G, Claverie, F, Pecheyran, C, Paroissin, C, Grignard, P-A, Motte, G, Chailan, O and Girard, J-P (2021b) Direct U–Pb dating of carbonates from micron-scale femtosecond laser ablation inductively coupled plasma mass spectrometry images using robust regression. Geochronology 3, 67–87.CrossRefGoogle Scholar
Hoareau, G, Crognier, N, Lacroix, B, Aubourg, C, Roberts, NMW, Niemi, N, Branellec, M, Beaudoin, N and Suarez Ruiz, I (2021a) Combination of Δ47 and U-Pb dating in tectonic calcite veins unravel the last pulses related to the Pyrenean Shortening (Spain). Earth and Planetary Science Letters 553, 116636.CrossRefGoogle Scholar
Holland, M, Saxena, N and Urai, JL (2009a) Evolution of fractures in a highly dynamic thermal, hydraulic, and mechanical system-(II) remote sensing fracture analysis, Jabal Shams, Oman Mountains. GeoArabia 14, 163–94.CrossRefGoogle Scholar
Holland, M and Urai, JL (2010) Evolution of anastomosing crack–seal vein networks in limestones: insight from an exhumed high-pressure cell, Jabal Shams, Oman Mountains. Journal of Structural Geology 32, 1279–90.CrossRefGoogle Scholar
Holland, M, Urai, JL, Muchez, P and Willemse, EJM (2009b) Evolution of fractures in a highly dynamic thermal, hydraulic, and mechanical system – (I) Field observations in Mesozoic Carbonates, Jabal Shams, Oman Mountains. GeoArabia 14, 57–110.CrossRefGoogle Scholar
Hollocher, K (1991) Prograde amphibole dehydration reactions during high-grade regional metamorphism, central Massachusetts, USA. American Mineralogist 76, 956–70.Google Scholar
Horita, J (2014) Oxygen and carbon isotope fractionation in the system dolomite–water–CO2 to elevated temperatures. Geochimica et Cosmochimica Acta 129, 111–24.CrossRefGoogle Scholar
Horton, BK, Capaldi, TN, Mackaman-Lofland, C, Perez, ND, Bush, MA, Fuentes, F and Constenius, KN (2022) Broken foreland basins and the influence of subduction dynamics, tectonic inheritance, and mechanical triggers. Earth-Science Reviews, 104193.CrossRefGoogle Scholar
Hough, BG, Fan, M and Passey, BH (2014) Calibration of the clumped isotope geothermometer in soil carbonate in Wyoming and Nebraska, USA: implications for paleoelevation and paleoclimate reconstruction. Earth and Planetary Science Letters 391, 110–20.CrossRefGoogle Scholar
Hu, G and Clayton, RN (2003) Oxygen isotope salt effects at high pressure and high temperature and the calibration of oxygen isotope geothermometers. Geochimica et Cosmochimica Acta 67, 3227–46.CrossRefGoogle Scholar
Hudec, MR and Jackson, MPA (2007) Terra infirma: understanding salt tectonics. Earth-Science Reviews 82, 1–28.CrossRefGoogle Scholar
Humphrey, E, Gomez-Rivas, E, Koehn, D, Bons, PD, Neilson, J, Martín-Martín, JD and Schoenherr, J (2019) Stylolite-controlled diagenesis of a mudstone carbonate reservoir: a case study from the Zechstein_2_Carbonate (Central European Basin, NW Germany). Marine and Petroleum Geology 109, 88–107.CrossRefGoogle Scholar
Huntington, KW, Budd, DA, Wernicke, BP and Eiler, JM (2011) Use of clumped-isotope thermometry to constrain the crystallization temperature of diagenetic calcite. Journal of Sedimentary Research 81, 656–69.CrossRefGoogle Scholar
Husson, JM, Higgins, JA, Maloof, AC and Schoene, B (2015) Ca and Mg isotope constraints on the origin of Earth’s deepest δ13C excursion. Geochimica et Cosmochimica Acta 160, 243–66.CrossRefGoogle Scholar
Irwin, H, Curtis, C and Coleman, M (1977) Isotopic evidence for source of diagenetic carbonates formed during burial of organic-rich sediments. Nature 269, 209–13.CrossRefGoogle Scholar
Jakubowicz, M, Agirrezabala, LM, Belka, Z, Siepak, M and Dopieralska, J (2022) Sr–Nd isotope decoupling at Cretaceous hydrocarbon seeps of the Basque-Cantabrian Basin (Spain): implications for tracing volcanic-influenced fluids in sedimented rifts. Marine and Petroleum Geology 135, 105430.CrossRefGoogle Scholar
Jin, XY, Zhao, JX, Feng, YX, Hofstra, AH, Deng, XD, Zhao, XF and Li, JW (2021) Calcite U-Pb dating unravels the age and hydrothermal history of the giant Shuiyindong carlin-type gold deposit in the Golden Triangle, South China. Economic Geology 116, 1253–65.CrossRefGoogle Scholar
Jonas, L, John, T, King, HE, Geisler, T and Putnis, A (2014) The role of grain boundaries and transient porosity in rocks as fluid pathways for reaction front propagation. Earth and Planetary Science Letters 386, 64–74.CrossRefGoogle Scholar
Jordan, TE and Allmendinger, RW (1986). The Sierras Pampeanas of Argentina: a modern analogue of Rocky Mountain foreland deformation. American Journal of Science 286, 737–64.CrossRefGoogle Scholar
Kareem, KH, Al-Aasm, IS and Mansurbeg, H (2019) Structurally-controlled hydrothermal fluid flow in an extensional tectonic regime: a case study of Cretaceous Qamchuqa Formation, Zagros Basin, Kurdistan Iraq. Sedimentary Geology 386, 52–78.CrossRefGoogle Scholar
Kergaravat, C, Ribes, C, Legeay, E, Callot, JP, Kavak, KS and Ringenbach, JC (2016) Minibasins and salt canopy in foreland fold-and-thrust belts: the central Sivas Basin, Turkey. Tectonics 35, 1342–66.CrossRefGoogle Scholar
Kim, ST and O’Neil, JR (1997) Equilibrium and nonequilibrium oxygen isotope effects in synthetic carbonates. Geochimica et Cosmochimica Acta 61, 3461–75.CrossRefGoogle Scholar
Kirkwood, D, Ayt-Ougougdal, M, Gayot, T, Beaudoin, G and Pironon, J (2000) Paleofluid-flow in a foreland basin, Northern Appalachians: from syntectonic flexural extension to Taconian overthrusting. Journal of Geochemical Exploration 69–70, 269–73.CrossRefGoogle Scholar
Kirschner, DL and Kennedy, LA (2001) Limited syntectonic fluid flow in carbonate-hosted thrust faults of the Front Ranges, Canadian Rockies, inferred from stable isotope data and structures. Journal of Geophysical Research: Solid Earth 106, 8827–40.CrossRefGoogle Scholar
Koehn, D, Rood, MP, Beaudoin, N, Chung, P, Bons, PD and Gomez-Rivas, E (2016) A new stylolite classification scheme to estimate compaction and local permeability variations. Sedimentary Geology 346, 60–71.CrossRefGoogle Scholar
Koeshidayatullah, A, Corlett, H, Stacey, J, Swart, PK, Boyce, and Hollis, C (2020b) Origin and evolution of fault-controlled hydrothermal dolomitization fronts: a new insight. Earth and Planetary Science Letters 541, 116291.CrossRefGoogle Scholar
Koeshidayatullah, A, Corlett, H, Stacey, J, Swart, PK, Boyce, A, Robertson, H, Whitaker, F and Hollis, C (2020a) Evaluating new fault-controlled hydrothermal dolomitization models: insights from the Cambrian Dolomite, Western Canadian Sedimentary Basin. Sedimentology 67, 2945–73.Google Scholar
Kylander-Clark, ARC (2020) Expanding the limits of laser-ablation U–Pb calcite geochronology. Geochronology 2, 343–54.CrossRefGoogle Scholar
Labeur, A, Beaudoin, NE, Lacombe, O, Emmanuel, L, Petracchini, L, Daëron, M, Klimowicz, S and Callot, JP (2021) Burial-deformation history of folded rocks unraveled by fracture analysis, stylolite paleopiezometry and vein cement geochemistry: a case study in the Cingoli Anticline (Umbria-Marche, Northern Apennines). Geosciences 11, 135.CrossRefGoogle Scholar
Lacombe, O (2010) Calcite twins, a tool for tectonic studies in thrust belts and stable orogenic forelands. Oil & Gas Science and Technology – Revue d’IFP Energies nouvelles 65, 809–38.CrossRefGoogle Scholar
Lacombe, O, Beaudoin, NE, Hoareau, G, Labeur, A, Pecheyran, C and Callot, JP (2021) Dating folding beyond folding, from layer-parallel shortening to fold tightening, using mesostructures: lessons from the Apennines, Pyrenees, and Rocky Mountains. Solid Earth 12, 2145–57.CrossRefGoogle Scholar
Lacombe, O and Bellahsen, N (2016) Thick-skinned tectonics and basement-involved fold-thrust belts: insights from selected Cenozoic orogens. Geological Magazine 153, 763–810.CrossRefGoogle Scholar
Lacombe, O and Mouthereau, F (1999) What is the real front of orogens? The Pyrenean orogen as a case study. Compte rendu de l’académie des sciences 329, 889–96.Google Scholar
Lacombe, O and Rolland, Y (2016) An introduction to the Special Issue on “Fluids in crustal deformation: fluid flow, fluid-rock interactions, rheology, melting and resources”. Journal of Geodynamics 101, 1–4.CrossRefGoogle Scholar
Lacombe, O, Swennen, R and Caracausi, A (2014) An introduction to the Special Issue on “Fluid-rock-tectonics interactions in basins and orogens”. Marine and Petroleum Geology 55, 1–5.CrossRefGoogle Scholar
Lacroix, B, Baumgartner, LP, Bouvier, AS, Kempton, PD and Vennemann, T (2018) Multi fluid-flow record during episodic mode I opening: a microstructural and SIMS study (Cotiella Thrust Fault, Pyrenees). Earth and Planetary Science Letters 503, 37–46.CrossRefGoogle Scholar
Lacroix, B, Buatier, M, Labaume, P, Trave, A, Dubois, M, Charpentier, D, Ventalon, S and Convert-Gaubier, D (2011) Microtectonic and geochemical characterization of thrusting in a foreland basin: example of the South-Pyrenean orogenic wedge (Spain). Journal of Structural Geology 33, 1359–77.CrossRefGoogle Scholar
Lacroix, B, Leclère, H, Buatier, M and Fabbri, O (2013) Weakening processes in thrust faults: insights from the Monte Perdido thrust fault (southern Pyrenees, Spain). Geofluids 13, 56–65.CrossRefGoogle Scholar
Lacroix, B, Trave, A, Buatier, M, Labaume, P, Vennemann, T and Dubois, M (2014) Syntectonic fluid-flow along thrust faults: example of the South-Pyrenean fold-and-thrust belt. Marine and Petroleum Geology 49, 84–98.CrossRefGoogle Scholar
Laubach, SE, Eichhubl, P, Hilgers, C and Lander, RH (2010) Structural diagenesis. Journal of Structural Geology 32, 1866–72.CrossRefGoogle Scholar
Laubach, SE, Lander, RH, Criscenti, LJ, Anovitz, LM, Urai, JL, Pollyea, RM, Hooker, JN, Narr, W, Evans, MA, Kerisit, SN, Olson, JE, Dewers, T, Fisher, D, Bodnar, R, Evans, B, Dove, P, Bonnell, LM, Marder, MP and Pyrak-Nolte, L (2019) The role of chemistry in fracture pattern development and opportunities to advance interpretations of geological materials. Reviews of Geophysics 57, 1065–111.CrossRefGoogle Scholar
Lee, YJ and Morse, JW (1999) Calcite precipitation in synthetic veins: implications for the time and fluid volume necessary for vein filling. Chemical Geology 156, 151–70.CrossRefGoogle Scholar
Lefticariu, L, Perry, EC, Fischer, MP and Banner, JL (2005) Evolution of fluid compartmentalization in a detachment fold complex. Geology 33, 69–72.CrossRefGoogle Scholar
Legeay, E, Ringenbach, JC, Kergaravat, C, Pichat, A, Mohn, G, Vergés, J, Sevki Kavak, K and Callot, JP (2020) Structure and kinematics of the Central Sivas Basin (Turkey): salt deposition and tectonics in an evolving fold-and-thrust belt. In Fold and Thrust Belts: Structural Style, Evolution and Exploration (ed. JA Hammerstein), pp. 361–96. Geological Society of London, Special Publication no. 490CrossRefGoogle Scholar
Lin, Y, Jochum, KP, Scholz, D, Hoffmann, DL, Stoll, B, Weis, U and Meinrat, OA (2017) In-situ high spatial resolution LA-MC-ICPMS 230Th/U dating enables detection of small-scale age inversions in speleothems. Solid Earth Sciences 2, 1–9.CrossRefGoogle Scholar
Lloyd, MK, Ryb, U and Eiler, JM (2018) Experimental calibration of clumped isotope reordering in dolomite. Geochimica et Cosmochimica Acta 242, 1–20.CrossRefGoogle Scholar
Lucca, A, Storti, F, Balsamo, F, Clemenzi, L, Fondriest, M, Burgess, R and Di Toro, G (2019) From submarine to subaerial out-of-sequence thrusting and gravity-driven extensional faulting: Gran Sasso Massif, central Apennines, Italy. Tectonics 38, 4155–84.CrossRefGoogle Scholar
Lynch, EA, Mulch, A, Yonkee, A and van der Pluijm, B (2019) Surface fluids in the evolving Sevier fold–thrust belt of ID–WY indicated by hydrogen isotopes in dated, authigenic clay minerals. Earth and Planetary Science Letters 513, e2021GC009868.CrossRefGoogle Scholar
Lynch, EA, Pană, D and van der Pluijm, BA (2021) Focusing fluids in faults: evidence from stable isotopic studies of dated clay-rich fault gouge of the Alberta Rockies. Geochemistry, Geophysics, Geosystems 22, e2021GC009868.CrossRefGoogle Scholar
Lynch, EA and van der Pluijm, B (2017) Meteoric fluid infiltration in the Argentine Precordillera fold-and-thrust belt: evidence from H isotopic studies of neoformed clay minerals. Lithosphere 9, 134–45.CrossRefGoogle Scholar
Lyons, JB and Snellenburg, J (1971) Dating faults. GSA Bulletin 82, 1749–52.CrossRefGoogle Scholar
MacDonald, JM, Faithfull, JW, Roberts, NMW, Davies, AJ, Holdsworth, CM. Newton, M, Williamson, S, Boyce, A and John, CM (2019) Clumped-isotope palaeothermometry and LA-ICP-MS U–Pb dating of lava-pile hydrothermal calcite veins. Contributions to Mineralogy and Petrology 174, 1–15.CrossRefGoogle Scholar
MacDonald, JM, John, CM and Girard, JP (2018) Testing clumped isotopes as a reservoir characterization tool: a comparison with fluid inclusions in a dolomitized sedimentary carbonate reservoir buried to 2–4 km. In From Source to Seep: Geochemical Applications of Hydrocarbon Systems (ed. M Lawson), pp. 189–202. Geological Society of London, Special Publication no. 468.Google Scholar
Machel, HG (1985a) Cathodoluminescence in calcite and dolomite and its chemical interpretation. Geoscience Canada 12, 139–47.Google Scholar
Machel, HG (1985b) Fibrous gypsum and fibrous anhydrite in veins. Sedimentology 32, 443–54.CrossRefGoogle Scholar
Machel, HG (1997) Recrystallization versus neomorphism, and the concept of “significant recrystallization” in dolomite research. Sedimentary Geology 113, 161–8.CrossRefGoogle Scholar
Machel, HG and Cavell, PA (1999) Low-flux, tectonically-induced squeegee fluid flow (“hot flash”) into the Rocky Mountain Foreland Basin. Bulletin of Canadian Petroleum Geology 47, 510–33.Google Scholar
Machel, HG and Lonnee, J (2002) Hydrothermal dolomite – a product of poor definition and imagination. Sedimentary Geology 152, 163–71.CrossRefGoogle Scholar
Mangenot, X, Bonifacie, M, Gasparrini, M, Götz, A, Chaduteau, C, Ader, M and Rouchon, V (2017) Coupling Δ47 and fluid inclusion thermometry on carbonate cements to precisely reconstruct the temperature, salinity and δ18O of paleo-groundwater in sedimentary basins. Chemical Geology 472, 44–57.CrossRefGoogle Scholar
Mangenot, X, Gasparrini, M, Rouchon, V and Bonifacie, M (2018) Basin-scale thermal and fluid flow histories revealed by carbonate clumped isotopes (Δ47) – Middle Jurassic carbonates of the Paris Basin depocentre. Sedimentology 65, 123–50.CrossRefGoogle Scholar
Marshak, S, Karlstom, K and Timmons, JM (2000) Inversion of Proterozoic extensional faults: an explanation for the pattern of Laramide and Ancestral Rockies intracratonic deformation, United States. Geology 28, 735–8.2.0.CO;2>CrossRefGoogle Scholar
Martín-Martín, JD, Gomez-Rivas, E, Bover-Arnal, T, Travé, A, Salas, R, Moreno-Bedmar, JA, Tomás, S, Corbella, M, Teixell, A, Vergés, J and Stafford, SL (2013) The Upper Aptian to Lower Albian syn-rift carbonate succession of the southern Maestrat Basin (Spain): facies architecture and fault-controlled stratabound dolostones. Cretaceous Research 41, 217–36.CrossRefGoogle Scholar
Martín-Martín, JD, Gomez-Rivas, E, Gómez-Gras, D, Travé, A, Ameneiro, R, Koehn, D and Bons, PD (2018) Activation of stylolites as conduits for overpressured fluid flow in dolomitized platform carbonates. Geological Society of London, Special Publications 459, 15776.CrossRefGoogle Scholar
McArthur, JM, Howarth, RJ and Bailey, TR (2001) Strontium isotope stratigraphy: LOWESS Version 3: best fit to the Marine Sr-Isotope Curve for 0–509 Ma and accompanying look-up table for deriving numerical age. The Journal of Geology 109, 155–70.CrossRefGoogle Scholar
McCaig, AM (1988) Deep fluid circulation in fault zones. Geology 16, 867–70.2.3.CO;2>CrossRefGoogle Scholar
McCaig, AM, Tritlla, J and Banks, DA (2000) Fluid flow patterns during Pyrenean thrusting. Journal of Geochemical Exploration 69–70, 539–43.CrossRefGoogle Scholar
Merino, E and Canals, À (2011) Self-accelerating dolomite-for-calcite replacement: self-organized dynamics of burial dolomitization and associated mineralization. American Journal of Science 311, 573–607.CrossRefGoogle Scholar
Micarelli, L, Benedicto, A and Wibberley, CAJ (2006) Structural evolution and permeability of normal fault zones in highly porous carbonate rocks. Journal of Structural Geology 28, 1214–27.CrossRefGoogle Scholar
Michael, K and Bachu, S (2001) Fluids and pressure distributions in the foreland-basin succession in the west-central part of the Alberta Basin, Canada: evidence for permeability barriers and hydrocarbon generation and migration. AAPG Bulletin 85, 1231–52.Google Scholar
Minissale, A, Magro, G, Martinelli, G, Vaselli, O and Tassi, GF (2000) Fluid geochemical transect in the Northern Apennines (central-northern Italy): fluid genesis and migration and tectonic implications. Tectonophysics 319, 199–222.CrossRefGoogle Scholar
Missenard, Y, Bertrand, A, Vergely, P, Benedicto, A, Cushing, ME and Rocher, M (2014) Fracture-fluid relationships: implications for the sealing capacity of clay layers – insights from field study of the Blue Clay formation, Maltese islands. Bulletin de la Société Géologique de France 185, 51–63.CrossRefGoogle Scholar
Moore, J, Beinlich, A, Porter, JK, Talavera, C, Berndt, J, Piazolo, S, Austrheim, H and Putnis, A (2020) Microstructurally controlled trace element (Zr, U–Pb) concentrations in metamorphic rutile: an example from the amphibolites of the Bergen Arcs. Journal of Metamorphic Geology 38, 103–27.CrossRefGoogle Scholar
Morad, S, Al-Aasm, IS, Sirat, M and Sattar, MM (2010) Vein calcite in Cretaceous carbonate reservoirs of Abu Dhabi: record of origin of fluids and diagenetic conditions. Journal of Geochemical Exploration 106, 156–70.CrossRefGoogle Scholar
Moragas, M, Martínez, C, Baqués, V, Playà, E, Travé, A, Alías, G and Cantarero, I (2013) Diagenetic evolution of a fractured evaporite deposit (Vilobí Gypsum Unit, Miocene, NE Spain). Geofluids 13, 180–93.CrossRefGoogle Scholar
Motte, G, Hoareau, G, Callot, JP, Revillon, S, Piccoli, F, Calassou, S and Gaucher, EC (2021) Rift and salt-related multi-phase dolomitization: example from the northwestern Pyrenees. Marine and Petroleum Geology 126, 104932.CrossRefGoogle Scholar
Mottram, CM, Kellett, DA, Barresi, T, Zwingmann, H, Friend, M, Todd, A and Percival, JB (2020) Syncing fault rock clocks: direct comparison of U-Pb carbonate and K-Ar illite fault dating methods. Geology 48, 1179–83.CrossRefGoogle Scholar
Mountjoy, EW, Qing, H and McNutt, RH (1992) Strontium isotopic composition of Devonian dolomites, Western Canada Sedimentary Basin: significance of sources of dolomitizing fluids. Applied Geochemistry 7, 59–75.CrossRefGoogle Scholar
Mourgues, R and Cobbold, PR (2003) Some tectonic consequences of fluid overpressures and seepage forces as demonstrated by sandbox modelling. Tectonophysics 376, 75–97.CrossRefGoogle Scholar
Mouthereau, F, Lacombe, O and Vergés, J (2012) Building the Zagros collisional orogen: timing, strain distribution and the dynamics of Arabia/Eurasia plate convergence. Tectonophysics 532–535, 27–60.CrossRefGoogle Scholar
Mouthereau, F, Tensi, J, Bellahsen, N, Lacombe, O, de Boisgrollier, T and Kargar, S (2007) Tertiary sequence of deformation in a thin-skinned/thick-skinned collision belt: the Zagros Folded Belt (Fars, Iran). Tectonics 26, TC5006.CrossRefGoogle Scholar
Mozafari, M, Swennen, R, Balsamo, F, Clemenzi, L, Storti, F, El Desouky, H, Vanhaecke, F, Tueckmantel, C, Solum, J and Taberner, C (2015) Palofluid evolution in fault-damage zones: evidence from fault-fold interaction events in the Jabal Qusaybah Anticline (Adam Foothills, North Oman). Journal of Sedimentary Research 85, 1525–51.CrossRefGoogle Scholar
Mozafari, M, Swennen, R, Balsamo, F, El Desouky, H, Storti, F and Taberner, C (2019) Fault-controlled dolomitization in the Montagna dei Fiori Anticline (Central Apennines, Italy): record of a dominantly pre-orogenic fluid migration. Solid Earth 10, 1355–83.CrossRefGoogle Scholar
Mozafari, M, Swennen, R, Muchez, P, Vassilieva, E, Balsamo, F, Storti, F, Pironon, J and Taberner, C (2017) Origin of the saline paleofluids in fault-damage zones of the Jabal Qusaybah Anticline (Adam Foothills, Oman): constraints from fluid inclusions geochemistry. Marine and Petroleum Geology 86, 537–46.CrossRefGoogle Scholar
Muñoz-López, D, Cruset, D, Vergés, J, Cantarero, I, Benedicto, A, Mangenot, X, Albert, R, Gerdes, A, Beranoaguirre, A and Travé, A (2022) Spatio-temporal variation of fluid flow behavior along a fold: the Bóixols-Sant Corneli anticline (Southern Pyrenees) from U–Pb dating and structural, petrographic and geochemical constraints. Marine and Petroleum Geology 143, 105788.CrossRefGoogle Scholar
Nardini, N, Muñoz-López, D, Cruset, D, Cantarero, I, Martín-Martín, JD, Benedicto, A, Gomez-Rivas, E, John, CM and Travé, A (2019) From early contraction to post-folding fluid evolution in the frontal part of the Bóixols Thrust Sheet (Southern Pyrenees) as revealed by the texture and geochemistry of calcite cements. Minerals 9, 117.CrossRefGoogle Scholar
Neely, TG and Erslev, EA (2009) The interplay of fold mechanisms and basement weaknesses at the transition between Laramide basement-involved arches, north-central Wyoming, USA. Journal of Structural Geology 31, 1012–27.CrossRefGoogle Scholar
Nelson, RA (1981) Significance of fracture sets associated with stylolite zones. AAPG Bulletin 65, 2417–25.Google Scholar
Nesbitt, BE and Muehlenbachs, K (1995) Geochemical studies of the origins and effects of synorogenic crustal fluids in the southern Omineca Belt of British Columbia, Canada. GSA Bulletin 107, 1033–50.2.3.CO;2>CrossRefGoogle Scholar
Nooitgedacht, CW, van der Lubbe, HJL, de Graaf, S, Ziegler, M, Staudigel, PT and Reijmer, JJG (2021) Restricted internal oxygen isotope exchange in calcite veins: constraints from fluid inclusion and clumped isotope-derived temperatures. Geochimica et Cosmochimica Acta 297, 24–39.CrossRefGoogle Scholar
Oliver, J (1986) Fluids expelled tectonically from orogenic belts: their role in hydrocarbon migration and other geologic phenomena. Geology 14, 99–102.2.0.CO;2>CrossRefGoogle Scholar
Oliver, NHS and Bons, PD (2001) Mechanisms of fluid flow and fluid-rock interaction in fossil metamorphic hydrothermal systems inferred from vein-wall rock patterns, geometry and microstructure. Geofluids 1, 137–62.CrossRefGoogle Scholar
Ortega, OJ, Gale, JFW and Marrett, R (2010) Quantifying diagenetic and stratigraphic controls on fracture intensity in platform carbonates: an example from the Sierra Madre Oriental, northeast Mexico. Journal of Structural Geology 32, 1943–59.CrossRefGoogle Scholar
Ortiz, JP, Person, MA, Mozley, PS, Evans, JP and Bilek, SL (2019) The role of fault-zone architectural elements on pore pressure propagation and induced seismicity. Groundwater 57, 465–78.CrossRefGoogle ScholarPubMed
Pagel, M, Bonifacie, M, Schneider, DA, Gautheron, C, Brigaud, B, Calmels, D, Cros, A, Saint-Bezar, B, Landrein, P, Sutcliffe, C, Davis, D and Chaduteau, C (2018) Improving paleohydrological and diagenetic reconstructions in calcite veins and breccia of a sedimentary basin by combining Δ47 temperature, δ18O water and U-Pb age. Chemical Geology 481, 1–17.CrossRefGoogle Scholar
Pană, DI and van der Pluijm, BA (2015) Orogenic pulses in the Alberta Rocky Mountains: radiometric dating of major faults and comparison with the regional tectono-stratigraphic record. GSA Bulletin 127, 480–502.Google Scholar
Paquette, J and Reeder, RJ (1995) Relationship between surface structure, growth mechanism, and trace element incorporation in calcite. Geochimica et Cosmochimica Acta 59, 735–49.CrossRefGoogle Scholar
Parekh, PP, Möller, P, Dulski, P and Bausch, WM (1977) Distribution of trace elements between carbonate and non-carbonate phases of limestone. Earth and Planetary Science Letters 34, 39–50.CrossRefGoogle Scholar
Parry, WT, Chan, MA and Beitler, B (2004) Chemical bleaching indicates episodes of fluid flow in deformation bands in sandstone. AAPG Bulletin 88, 175–91.CrossRefGoogle Scholar
Peckmann, J and Thiel, V (2004) Carbon cycling at ancient methane-seeps. Chemical Geology 205, 443–67.CrossRefGoogle Scholar
Pedrosa, ET, Boeck, L, Putnis, CV and Putnis, A (2017) The replacement of a carbonate rock by fluorite: kinetics and microstructure. American Mineralogist 102, 126–34.CrossRefGoogle Scholar
Petrus, K and Szymczak, P (2016) Influence of layering on the formation and growth of solution pipes. Frontiers in Physics 3, 1–13.CrossRefGoogle Scholar
Pfiffner, OA. (2017) Thick-skinned and thin-skinned tectonics: a global perspective. Geosciences 7, 71.CrossRefGoogle Scholar
Pichat, A, Hoareau, G, Callot, J-P, Legeay, E, Kavak, KS, Révillon, S, Parat, C and Ringenbach, J-C (2018) Evidence of multiple evaporite recycling processes in a salt-tectonic context, Sivas Basin, Turkey. Terra Nova 30, 40–9.CrossRefGoogle Scholar
Pichat, A, Hoareau, G, Callot, J-P and Ringenbach, J-C (2016) Diagenesis of Oligocene continental sandstones in salt-walled mini-basins – Sivas Basin, Turkey. Sedimentary Geology 339, 13–31.CrossRefGoogle Scholar
Pik, R and Marty, B (2009) Helium isotopic signature of modern and fossil fluids associated with the Corinth rift fault zone (Greece): implication for fault connectivity in the lower crust. Chemical Geology 266, 67–75.CrossRefGoogle Scholar
Pironon, J and Bourdet, J (2008) Petroleum and aqueous inclusions from deeply buried reservoirs: experimental simulations and consequences for overpressure estimates. Geochimica et Cosmochimica Acta 72, 4916–28.CrossRefGoogle Scholar
Qing, H and Mountjoy, E (1992) Large-scale fluid flow in the Middle Devonian Presqu’ile barrier, western Canada sedimentary basin. Geology 20, 903–6.Google Scholar
Ramsey, DW and Onasch, CM (1999) Fluid migration in a cratonic setting: the fluid histories of two fault zones in the eastern midcontinent. Tectonophysics 305, 307–23.CrossRefGoogle Scholar
Rasbury, ET and Cole, JM (2009) Directly dating geologic events: U-Pb dating of carbonates. Reviews of Geophysics 47, RG3001.CrossRefGoogle Scholar
Reeder, RJ and Grams, JC (1987) Sector zoning in calcite cement crystals: implications for trace element distributions in carbonates. Geochimica et Cosmochimica Acta 51, 187–94.CrossRefGoogle Scholar
Regnet, JB, David, C, Robion, P and Menéndez, B (2019) Microstructures and physical properties in carbonate rocks: a comprehensive review. Marine and Petroleum Geology 103, 366–76.CrossRefGoogle Scholar
Roberts, NMW, Drost, K, Horstwood, MSA, Condon, DJ, Chew, D, Drake, H, Milodowski, AE, McLean, NM, Smye, AJ, Walker, RJ, Haslam, R, Hodson, K, Imber, J, Beaudoin, N and Lee, JK (2020) Laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) U–Pb carbonate geochronology: strategies, progress, and limitations. Geochronology 2, 33–61.CrossRefGoogle Scholar
Roberts, NMW and Holdsworth, RE (2022) Timescales of faulting through calcite geochronology: a review. Journal of Structural Geology 158, 104578.CrossRefGoogle Scholar
Roberts, NMW, Žák, J, Vacek, F and Sláma, J (2021) No more blind dates with calcite: fluid-flow vs. fault-slip along the Očkov thrust, Prague Basin. Geoscience Frontiers 12, 101143.CrossRefGoogle Scholar
Roedder, E (1984) Fluid Inclusions: An Introduction to Studies of All Types of Fluid Inclusions, Gas, Liquid, or Melt, Trapped in Materials from Earth and Space, and Their Application to the Understanding of Geologic Processes, Volume 12, 644 pp. Washington, DC: Mineralogical Society of America.Google Scholar
Rosasco, G, Roedder, E and Simmons, JH (1975) Laser-excited Raman spectroscopy for nondestructive partial analysis of individual phases in fluid inclusions in minerals. Science 190, 557–60.CrossRefGoogle Scholar
Roure, F, Andriessen, P, Callot, JP, Faure, JL, Ferket, H, Gonzales, E, Guilhaumou, N, Lacombe, O, Malandain, J, Sassi, W, Schneider, F, Swennen, R and Vilasi, N (2010) The use of palaeo-thermo-barometers and coupled thermal, fluid flow and pore-fluid pressure modelling for hydrocarbon and reservoir prediction in fold and thrust belts. In Hydrocarbons in Contractional Belts (eds Goffey, G, Craig, J, Needham, T and Scott, R), pp. 87–114. Geological Society of London, Special Publication no. 348.Google Scholar
Roure, F, Swennen, R, Schneider, F, Faure, JL, Ferket, H, Guilhaumou, N, Osadetz, K, Robion, P and Vandeginste, V (2005) Incidence and importance of tectonics and natural fluid migration on reservoir evolution in foreland fold-and-thrust belts. Oil & Gas Science and Technology 60, 67–106.CrossRefGoogle Scholar
Rye, DM and Bradbury, HJ (1988) Fluid flow in the crust: an example from a Pyrenean thrust ramp. American Journal of Science 288, 197–235.CrossRefGoogle Scholar
Sachau, T, Bons, PD and Gomez-Rivas, E (2015) Transport efficiency and dynamics of hydraulic deformation networks. Frontiers in Physics 3, 1–13.CrossRefGoogle Scholar
Sassi, W, Guiton, MLE, Leroy, YM, Daniel, JM and Callot, JP (2012) Constraints on bed scale fracture chronology with a FEM mechanical model of folding: the case of Split Mountain (Utah, USA). Tectonophysics 576–577, 197–215.CrossRefGoogle Scholar
Scheiber, T, Viola, G, van der Lelij, R, Margreth, A and Schönenberger, J (2019) Microstructurally-constrained versus bulk fault gouge K-Ar dating. Journal of Structural Geology 127, 103868.CrossRefGoogle Scholar
Schneider, F (2003) Basin modeling in complex area: examples from eastern Venezuelan and Canadian Foothills. Oil & Gas Science and Technology 58, 313–24.CrossRefGoogle Scholar
Scisciani, V, Agostini, S, Calamita, F, Pace, P, Cilli, A, Giori, I and Paltrinieri, W (2014) Positive inversion tectonics in foreland fold-and-thrust belts: a reappraisal of the Umbria-Marche Northern Apennines (Central Italy) by integrating geological and geophysical data. Tectonophysics 637, 218–37.CrossRefGoogle Scholar
Scisciani, V, Patruno, S, Tavarnelli, E, Calamita, F, Pace, P and Iacopini, D (2019) Multi-phase reactivations and inversions of Paleozoic–Mesozoic extensional basins during the Wilson cycle: case studies from the North Sea (UK) and the Northern Apennines (Italy). In Fifty Years of the Wilson Cycle Concept in Plate Tectonics (eds RW Wilson, GA Houseman, KJW McCaffrey, AG Dore and SJH Butler), pp. 205–43. Geological Society of London, Special Publication no. 470.CrossRefGoogle Scholar
Segnit, ER, Holland, HD and Biscardi, CJ (1962). The solubility of calcite in aqueous solutions – I. The solubility of calcite in water between 75° and 200° at CO2 pressures up to 60 atm. Geochimica et Cosmochimica Acta 26, 1301–31.CrossRefGoogle Scholar
Sheppard, SMF (1986) Characterization and isotopic variations in natural waters. Reviews in Mineralogy, 16, 165–83.Google Scholar
Shields, GA and Webb, GE (2004) Has the REE composition of seawater changed over geological time? Chemical Geology 204, 103–7.CrossRefGoogle Scholar
Sibson, RH (1990) Conditions for fault-valve behaviour. In Deformation Mechanisms, Rheology and Tectonics (ed. Knipe, RJ), pp. 15–28. Geological Society of London, Special Publication no. 54.Google Scholar
Sibson, RH (2000) Fluid involvement in normal faulting. Journal of Geodynamics 29, 469–99.CrossRefGoogle Scholar
Sibson, RH (2005) Hinge-parallel fluid flow in fold-thrust belts: how widespread? Proceedings of the Geologists’ Association 116, 301–9.CrossRefGoogle Scholar
Sibuet, JC, Srivastava, SP and Spakman, W (2004) Pyrenean orogeny and plate kinematics. Journal of Geophysical Research: Solid Earth 109, 1–18.CrossRefGoogle Scholar
Smeraglia, L, Aldega, L, Bernasconi, SM, Billi, A, Boschi, C, Caracausi, A, Carminati, E, Franchini, S, Rizzo, AL, Rossetti, F and Vignaroli, G (2020b) The role of trapped fluids during the development and deformation of a carbonate/shale intra-wedge tectonic mélange (Mt. Massico, Southern Apennines, Italy). Journal of Structural Geology 138, 104086.CrossRefGoogle Scholar
Smeraglia, L, Bernasconi, SM, Berra, F, Billi, A, Boschi, C, Caracausi, A, Carminati, E, Castorina, F, Doglioni, C, Italiano, F, Rizzo, AL, Uysal, IT and Zhao, JX (2018) Crustal-scale fluid circulation and co-seismic shallow comb-veining along the longest normal fault of the central Apennines, Italy. Earth and Planetary Science Letters 498, 152–68.CrossRefGoogle Scholar
Smeraglia, L, Fabbri, O, Choulet, F, Buatier, M, Boulvais, P, Bernasconi, SM and Castorina, F (2019) Syntectonic fluid flow and deformation mechanisms within the frontal thrust of foreland fold-and-thrust belt: example from the Internal Jura, Eastern France. Tectonophysics 778, 228178.Google Scholar
Smeraglia, L, Fabbri, O, Choulet, F, Buatier, M, Boulvais, P, Bernasconi, SM and Castorina, F (2020a) Syntectonic fluid flow and deformation mechanisms within the frontal thrust of a foreland fold-and-thrust belt: example from the Internal Jura, Eastern France. Tectonophysics 778, 228178.CrossRefGoogle Scholar
Smeraglia, L, Giuffrida, A, Grimaldi, S, Pullen, A, La Bruna, V, Billi, A and Agosta, F (2021) Fault-controlled upwelling of low-T hydrothermal fluids tracked by travertines in a fold-and-thrust belt, Monte Alpi, Southern Apennines, Italy. Journal of Structural Geology 144, 104276.CrossRefGoogle Scholar
Stel, H (2009) Diagenetic crystallization and oxidation of siderite in red bed (Buntsandstein) sediments from the Central Iberian Chain, Spain. Sedimentary Geology 213, 89–96.CrossRefGoogle Scholar
Stolper, DA and Eiler, JM (2015) The kinetics of solid-state isotope-exchange reactions for clumped isotopes: a study of inorganic calcites and apatites from natural and experimental samples. American Journal of Science 315, 363–411.CrossRefGoogle Scholar
Stone, DS (1967) Theory of Paleozoic oil and gas accumulation in Bighorn Basin, Wyoming. AAPG Bulletin 51, 2056–114.Google Scholar
Su, A, Chen, H, Feng, Y-X, Zhao, JX, Wang, Z, Hu, M, Jiang, H and Duc Nguyen, A (2022) In situ U-Pb dating and geochemical characterization of multi-stage dolomite cementation in the Ediacaran Dengying Formation, Central Sichuan Basin, China: constraints on diagenetic, hydrothermal and paleo-oil filling events. Precambrian Research 368, 106481.CrossRefGoogle Scholar
Sutherland, R, Toy, VG, Townend, J, Cox, SC, Eccles, JD, Faulkner, DR, Prior, DJ, Norris, RJ, Mariani, E, Boulton, C, Carpenter, BM, Menzies, CD, Little, TA, Hasting, M, De Pascale, GP, Langridge, RM, Scott, HR, Reid Lindroos, Z, Fleming, B and Kopf, J (2012) Drilling reveals fluid control on architecture and rupture of the Alpine Fault, New Zealand. Geology 40, 1143–6.CrossRefGoogle Scholar
Swanson, EM, Wernicke, BP, Eiler, JM and Losh, S (2012) Temperatures and fluids on faults based on carbonate clumped-isotope thermometry. American Journal of Science 312, 1–21.CrossRefGoogle Scholar
Swart, PK (2015) The geochemistry of carbonate diagenesis: the past, present and future. Sedimentology 62, 1233–304.CrossRefGoogle Scholar
Swart, PK, Burns, SJ and Leder, JJ (1991) Fractionation of the stable isotopes of oxygen and carbon in carbon dioxide during the reaction of calcite with phosphoric acid as a function of temperature and technique. Chemical Geology: Isotope Geoscience section 86, 89–96.Google Scholar
Swennen, R, Muskha, K and Roure, F (2000) Fluid circulation in the Ionian fold and thrust belt (Albania): implications for hydrocarbon prospectivity. 70, 629–34.CrossRefGoogle Scholar
Szymczak, P and Ladd, AJC (2009) Wormhole formation in dissolving fractures. Journal of Geophysical Research: Solid Earth 114, 1–22.CrossRefGoogle Scholar
Szymczak, P and Ladd, AJC (2014) Reactive-infiltration instabilities in rocks. Part 2. Dissolution of a porous matrix. Journal of Fluid Mechanics 738, 591–630.CrossRefGoogle Scholar
Tang, J, Dietzel, M, Böhm, F, Köhler, SJ and Eisenhauer, A (2008) Sr2+/Ca2+ and 44Ca/40Ca fractionation during inorganic calcite formation: II. Ca isotopes. Geochimica et Cosmochimica Acta 72, 3733–45.CrossRefGoogle Scholar
Tang, J, Dietzel, M, Fernandez, A, Tripati, AK and Rosenheim, BE (2014) Evaluation of kinetic effects on clumped isotope fractionation (Δ47) during inorganic calcite precipitation. Geochimica et Cosmochimica Acta 134, 120–36.CrossRefGoogle Scholar
Tavani, S, Storti, F, Lacombe, O, Corradetti, A, Muñoz, JA and Mazzoli, S (2015) A review of deformation pattern templates in foreland basin systems and fold-and-thrust belts: implications for the state of stress in the frontal regions of thrust wedges. Earth-Science Reviews 141, 82–104.CrossRefGoogle Scholar
Thacker, JO and Karlstrom, KE (2019) U-Pb dating of calcite veins reveals complex stress evolution and thrust sequence in the Bighorn Basin, Wyoming, USA. Geology 47, e480.CrossRefGoogle Scholar
Tondi, E, Antonellini, M, Aydin, A, Marchegiani, L and Cello, G (2006) The role of deformation bands, stylolites and sheared stylolites in fault development in carbonate grainstones of Majella Mountain, Italy. Journal of Structural Geology 28, 376–91.CrossRefGoogle Scholar
Tonguç Uysal, I, Zhao, J-X, Golding, SD, Lawrence, MG, Glikson, M and Collerson, KD (2007) Sm-Nd dating and rare-earth element tracing of calcite: implications for fluid-flow events in the Bowen Basin, Australia. Chemical Geology 238, 63–71.CrossRefGoogle Scholar
Tostevin, R, Bradbury, HJ, Shields, GA, Wood, RA, Bowyer, F, Penny, AM and Turchyn, AV (2019) Calcium isotopes as a record of the marine calcium cycle versus carbonate diagenesis during the late Ediacaran. Chemical Geology 529, 119319.CrossRefGoogle Scholar
Toussaint, R, Aharonov, E, Koehn, D, Gratier, JP, Ebner, M, Baud, P, Rolland, A and Renard, F (2018) Stylolites: a review. Journal of Structural Geology 114, 163–95.CrossRefGoogle Scholar
Travé, A, Calvet, F, Sans, M, Verges, J and Thirlwall, M (2000) Fluid history related to the Alpine compression at the margin of the south-Pyrenean Foreland basin: the El Guix anticline. Tectonophysics 321, 73–102.CrossRefGoogle Scholar
Travé, A, Labaume, P, Calvet, F and Soler, A (1997) Sediment dewatering and pore fluid migration along thrust faults in a foreland basin inferred from isotopic and elemental geochemical analyses (Eocene southern Pyrenees, Spain). Tectonophysics 282, 375–98.CrossRefGoogle Scholar
Travé, A, Labaume, P and Vergés, J (2007) Fluid systems in foreland fold-and-thrust belts: an overview from the Southern Pyrenees. In Thrust Belts and Foreland Basins. Frontiers in Earth Sciences (eds O Lacombe, F Roure, J Lavé and J Vergés) Heidelberg: Springer, Berlin. https://doi.org/10.1007/978-3-540-69426-7_5.Google Scholar
Uysal, IT, Feng, YX, Zhao, JX, Isik, V, P, Nuriel and SD, Golding (2009). Hydrothermal CO2 degassing in seismically active zones during the late Quaternary. Chemical Geology 265, 442–54.CrossRefGoogle Scholar
van der Pluijm, BA, Craddock, JP, Graham, BR and Harris, JH (1997) Paleostress in cratonic North America: implications for deformation of continental interiors. Science 277, 794–6.CrossRefGoogle Scholar
van der Pluijm, BA, Hall, CM, Vrolijk, PJ, Pevear, DR and Covey, MC (2001) The dating of shallow faults in the Earth’s crust. Nature 412, 172–5.CrossRefGoogle ScholarPubMed
van der Pluijm, BA, Vrolijk, PJ, Pevear, DR, Hall, CM and Solum, J (2006) Fault dating in the Canadian Rocky Mountains: evidence for late Cretaceous and early Eocene orogenic pulses. Geology 34, 837–40.CrossRefGoogle Scholar
van Geet, M, Swennen, R, Durmishi, C, Roure, F and Muchez, PH (2002) Paragenesis of Cretaceous to Eocene carbonate reservoirs in the Ionian fold and thrust belt (Albania): relation between tectonism and fluid flow. Sedimentology 49, 697–718.CrossRefGoogle Scholar
Vandeginste, V, Swennen, R, Allaeys, M, Ellam, RM, Osadetz, K and Roure, F (2012) Challenges of structural diagenesis in foreland fold-and-thrust belts: a case study on paleofluid flow in the Canadian Rocky Mountains West of Calgary. Marine and Petroleum Geology 35, 235–51.CrossRefGoogle Scholar
Vannucchi, P, Remitti, F, Bettelli, G, Boschi, C and Dallai, L (2010) Fluid history related to the early Eocene-middle Miocene convergent system of the Northern Apennines (Italy): constraints from structural and isotopic studies. Journal of Geophysical Research: Solid Earth 115, 5405.CrossRefGoogle Scholar
Vass, A, Koehn, D, Toussaint, R, Ghani, I and Piazolo, S (2014) The importance of fracture-healing on the deformation of fluid-filled layered systems. Journal of Structural Geology 67, 94–106.CrossRefGoogle Scholar
Vignaroli, G, Rossetti, F, Petracchini, L, Argante, V, Bernasconi, SM, Brilli, M, Giustini, F, Yu, T-L, Shen, C-C and Soligo, M (2022) Middle Pleistocene fluid infiltration with 10–15 ka recurrence within the seismic cycle of the active Monte Morrone Fault System (central Apennines, Italy) Tectonophysics 827, 229269. doi: 10.1016/j.tecto.2022.229269.CrossRefGoogle Scholar
Vilasi, N, Malandain, J, Barrier, L, Callot, JP, Amrouch, K, Guilhaumou, N, Lacombe, O, Muska, K, Roure, F and Swennen, R (2009) From outcrop and petrographic studies to basin-scale fluid flow modelling: the use of the Albanian natural laboratory for carbonate reservoir characterisation. Tectonophysics 474, 367–92.CrossRefGoogle Scholar
Vilasi, N, Swennen, R and Roure, F (2006) Diagenesis and fracturing of Paleocene–Eocene carbonate turbidite systems in the Ionian Basin: the example of the Kelçyra area (Albania). Journal of Geochemical Exploration 89, 409–13.CrossRefGoogle Scholar
Villemant, B and Feuillet, N (2003) Dating open systems by the 238U–234U–230Th method: application to Quaternary reef terraces. Earth and Planetary Science Letters 210, 105–18.CrossRefGoogle Scholar
Viola, G, Zwingmann, H, Mattila, J and Käpyaho, A (2013) K-Ar illite age constraints on the Proterozoic formation and reactivation history of a brittle fault in Fennoscandia. Terra Nova 25, 236–44.CrossRefGoogle Scholar
Wacker, U, Fiebig, J, Tödter, J, Schöne, BR, Bahr, A, Friedrich, O, Tütken, T, Gischler, E and Joachimski, MM (2014) Empirical calibration of the clumped isotope paleothermometer using calcites of various origins. Geochimica et Cosmochimica Acta 141, 127–44.CrossRefGoogle Scholar
Wang, X, Gao, J, He, S, He, Z, Zhou, Y, Tao, Z, Zhang, J and Wang, Y (2017) Fluid inclusion and geochemistry studies of calcite veins in Shizhu synclinorium, central China: record of origin of fluids and diagenetic conditions. Journal of Earth Science 28, 315–32.CrossRefGoogle Scholar
Weber, J, Cheshire, MC, Bleuel, M, Mildner, D, Chang, YJ, Ievlev, A, Littrell, KC, Ilavsky, J, Stack, AG and Anovitz, LM (2021) Influence of microstructure on replacement and porosity generation during experimental dolomitization of limestones. Geochimica et Cosmochimica Acta 303, 137–58.CrossRefGoogle Scholar
Wennberg, OP, Casini, G, Jonoud, S and Peacock, DCP (2016) The characteristics of open fractures in carbonate reservoirs and their impact on fluid flow: a discussion. Petroleum Geoscience 22, 91–104.CrossRefGoogle Scholar
Xu, WG, Fan, HR, Hu, FF, Santosh, M, Yang, KF, Lan, TG and Wen, BJ (2015) Geochronology of the Guilaizhuang gold deposit, Luxi Block, eastern North China Craton: constraints from zircon U–Pb and fluorite-calcite Sm–Nd dating. Ore Geology Reviews 65, 390–9.CrossRefGoogle Scholar
Yan, H, Dreybrodt, W, Bao, H, Peng, Y, Wei, Y, Ma, S, Mo, B, Sun, H and Liu, Z (2021) The influence of hydrodynamics on the carbon isotope composition of inorganically precipitated calcite. Earth and Planetary Science Letters 565, 116932.CrossRefGoogle Scholar
Yardley, BWD and Graham, JT (2002) The origins of salinity in metamorphic fluids. Geofluids 2, 249–56.CrossRefGoogle Scholar
Yonkee, WA and Weil, AB (2015) Tectonic evolution of the Sevier and Laramide belts within the North American Cordillera orogenic system. Earth-Science Reviews 150, 531–93.CrossRefGoogle Scholar
Zaarur, S, Affek, HP and Brandon, MT (2013) A revised calibration of the clumped isotope thermometer. Earth and Planetary Science Letters 382, 47–57.CrossRefGoogle Scholar
Zeebe, RE (2007) An expression for the overall oxygen isotope fractionation between the sum of dissolved inorganic carbon and water. Geochemistry, Geophysics, Geosystems 8, Q09002.CrossRefGoogle Scholar
Zheng, Y-F (1999) Oxygen isotope fractionation in carbonate and sulfate minerals. Geochemical Journal 33, 109–26.CrossRefGoogle Scholar
Zuluaga, LF, Rotevatn, A, Keilegavlen, E and Fossen, H (2016) The effect of deformation bands on simulated fluid flow within fault-propagation fold trap types: lessons from the San Rafael monocline, Utah. AAPG Bulletin 100, 1523–40.CrossRefGoogle Scholar
Zwingmann, H, Offler, R, Wilson, T and Cox, SF (2004) K–Ar dating of fault gouge in the northern Sydney Basin, NSW, Australia: implications for the breakup of Gondwana. Journal of Structural Geology 26, 2285–95.CrossRefGoogle Scholar