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Upper Permian-Lower Cretaceous clay mineralogy of East Greenland: provenance, palaeoclimate and volcanicity

Published online by Cambridge University Press:  09 July 2018

H. Lindgreen  and
F. Surlyk
H. Lindgreen*
Affiliation:
, Clay Mineralogical Laboratory, Geological Survey of Denmark and Greenland, Thoravej 8, DK 2400 Copenhagen NV
F. Surlyk
Affiliation:
Geological Institute, University of Copenhagen, Øster Voldgade 10, DK 1350 Copenhagen K, Denmark
*
*E-mail: hl@geus.dk
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Abstract

The clay mineralogy of Upper Permian–Lower Cretaceous mudstones from East Greenland has been investigated by X-ray diffraction (XRD), atomic force microscopy (AFM) and thermal analysis in order to evaluate long-term trends in provenance and palaeoclimate and to detect possible volcanic events. The Upper Permian–Lower Triassic mudstones contain illite, chlorite, vermiculite, kaolinite and illite-smectite (I-S), whereas the Rhaetian–Sinemurian mudstones are dominated by kaolinite. Aalenian–Albian mudstones contain kaolinite and large amounts of I-S with ˜80% illite layers. Exceptions are three Kimmeridgian samples, which contain mainly I-S with 30% illite layers, and three Upper Barremian–Lower Aptian samples with large amounts of smectite layers. Discrete clay minerals in the Upper Permian–Jurassic mudstones are largely detrital. The smectite-rich I-S probably reflects episodes of volcanic activity in late Jurassic and late Barremian–early Aptian times. This is the first indication of Mesozoic volcanism from the Mesozoic rift basin of East Greenland. The main sediment source during late Permian–early Cretaceous times was weathered Precambrian and Caledonian crystalline basement. The only possibly climate-induced change is a change from chlorite, illite, vermiculite and kaolinite in Upper Permian–Lower Triassic mudstones to kaolinite and I-S in the Jurassic mudstones and is probably due to an increase in precipitation.

Keywords

clay mineralogy, East Greenland, volcanism, palaeoclimate, Permian, Jurassic, Cretaceous
Type
Research Article
Information
Clay Minerals , Volume 35 , Issue 5 , December 2000 , pp. 791 - 806
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2000

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References

Anderson, J.U. (1963) An improved pretreatment for mineralogical analysis of samples containing organic matter. Clays Clay Miner. 10, 380–388.CrossRefGoogle Scholar
Barshad, I. (1966) The effect of variation in precipitation on the nature of clay mineral formation in soils from acid and basic igneous rocks. Proc. Int. Clay Conf., 1966, Jerusalem, 167-173.Google Scholar
Bradshaw, M.J. (1975) Origin of montmorillonite bands in the Middle Jurassic of eastern England. Earth Planet. Sci. Lett. 26, 245–252.Google Scholar
Chamley, H., Debrabant, P., Candillier, A.-M. & Foulon, J. (1983) Clay mineralogy and inorganic geochemical stratigraphy of Blake-Bahama Basin since the Callovian, site 534, Deep Sea Drilling Project leg 76. Init. Rep. DSDP. 76, 437–451.Google Scholar
Chowdhury, A.N. (1982) Smectite, zeolite, biotite and apatite in the Corallian (Oxfordian) sediments of the Baulking area in Berkshire, England. Geol. Mag. 119, 487–496.CrossRefGoogle Scholar
Clemmensen, L.B. (1978) Alternating aeolian, sabhka and shallow-lake deposits from the Middle Triassic Gipsdalen Format ion, Scoresby Land, East Greenland. Palaeogeogr., Palaeoclimatol., Palaeoecol. 24, 111–135.Google Scholar
Clemmensen, L., Kent, D.V. & Jenkins, F.A. Jr. (1998) A late Triassic lake system in East Greenland: facies, depositional cycles and palaeoclimate. Palaeogeogr., Palaeoclimatol., Palaeoecol. 140, 135–157.Google Scholar
Cowperthwaite, I.A., Fitch, F.J., Miller, J.A., Mitchell, J.G. & Robertson, R.H.S. (1972) Sedimentation, petrogenesis and radioisotopic age of the Cretaceous Fuller's Earth of Southern England. Clay Miner. 9, 309–327.Google Scholar
Dalland, A. & Thusu, B. (1977) Kimmeridgian volcanic ash in Andoya, Northern Norway. Pp. 1–14 in: Mesozoic Northern North Sea Symposium. Norwegian Petroleum Society, Oslo.Google Scholar
Dam, G. & Surlyk, F. (1993) Cyclic sedimentation in a large wave and storm-dominated anoxic lake, Kap Stewart Formation (Rhaetian-Sinemurian), Jameson Land, East Greenland. Pp. 419–448 in: Sequence Stratigraphy and Facies Associations (Posamentier, H.W., Summerhayes, D.P., Haq, B.U. & Allen, G.P., editors ). Special Publications of the International Association of Sedimentologists, 18.Google Scholar
Dam, G. & Surlyk, F. (1998) Stratigraphy of the Neill Klinter Group; a Lower-Middle Jurassic tidal embayment succession, Jameson Land, East Greenland. Bull. Grønlands geol. Unders. 175, 1–80.Google Scholar
Deconinck, J.F. & Chamley, H. (1995) Diversity of smectite origins in Late Cretaceous sediments: examples of chalks from Northern France. Clay Miner. 30, 365–379.CrossRefGoogle Scholar
Deconinck, J.-F., Beaudoin, B., Chamley, H., Joseph, P. & Raoult, J.F. (1985) Contrôles techtonique, eustatique et climatique de la sédimentation argileuse du domaine subalpin français au Malm-Crétacé. Rev. Géol. Dyn. Géogr. Phys. 26, 311–320.Google Scholar
Doré, A.G. (1991) The structural foundation and evolution of Mesozoic seaways between Europe and the Arctic. Palaeogeogr., Palaeoclimatol., Palaeoecol. 87, 441–492.CrossRefGoogle Scholar
Drits, V.A., Lindgreen, H., Salyn, A.L., Ylagan, R. & McCarty, D.K. (1998) Semiquantitative determination o. trans-vacant and cis-vacant 2:1 layers in illites and illite-smectites by thermal analysis and X-ray diffraction. Am. Miner. 83, 1188–1198.Google Scholar
Engkilde, M. & Surlyk, F. (in press) Sequence stratigraphy of the Middle Jurassic shallow marine Vardekløft Group, East Greenland. In: The Jurassic of Denmark and Greenland (Surlyk, F. & Ineson, J.R., editors). Geology Denmark Surv. Bull.Google Scholar
Foscolos, A.E., Powell, T.G. & Gunther, P.R. (1976) The use of clay minerals and inorganic and organic geochemical indicators for evaluating the degree of diagenesis and oil generating potential of shales. Geochim. Cosmochim. Acta. 40, 953–966.Google Scholar
Frey, M. (1970) The step from diagenesis to metamorphism in pelitic rocks during Alpine orogenesis. Sedimentology. 15, 261–279.Google Scholar
Hallam, A. & Sellwood, B.W. (1968) Origin of Fuller's Earth in the Mesozoic of Southern England. Nature. 220, 1193–1195.Google Scholar
Hallam, A., Grose, J.A. & Ruffell, A.H. (1991) Palaeoclimatic significance of changes in clay mineralogy across the Jurassic-Cretaceous boundary in England and France. Palaeogeogr., Palaeoclimatol., Palaeoecol. 81, 173–187.Google Scholar
Hansen, P.L. & Lindgreen, H. (1989) Mixed-layer illite/smectite diagenesis in Upper Jurassic claystones from the North Sea and onshore Denmark. Clay Miner. 24, 197–213.Google Scholar
Hower, J., Eslinger, E.V., Hower, M.E. & Perry, E.A. (1976) Mechanism of burial metamorphism of argillaceous sediment: 1. Mineralogical and chemical evidence. Bull. Geol. Soc. Am. 87, 725–737.Google Scholar
Howitt, F., Aston, E.R. & Jaqué, M. (1975) The occurrence of Jurassic volcanics in the North Sea. Pp. 379–387 in: Petroleum and the Continental shelf of North-West Europe 1, (Woodland, A.W., editor). Applied Science Publishers, London.Google Scholar
Hurst, A. (1985) The implications of clay mineralogy to palaeoclimate and provenance during the Jurassic in NE Scotland. Scot. J. Geol. 21, 143–160.Google Scholar
Jeans, C.V., Merriman, R.J., Mitchell, J.G. & Bland, D.J. (1982) Volcanic clays in the Cretaceous of Southern England and Northern Ireland. Clay Miner. 17, 105–156.Google Scholar
Knox, R.W.O'B. (1977) Upper Jurassic pyroclastic rocks in Skye, west Scotland. Nature. 265, 323–324.Google Scholar
Knox, R. W. O'B. & Fletcher, B.N. (1978) Bentonites in the lower D beds (Ryazanian) of the Speeton Clay of Yorkshire. Proc. Yorks. Geol. Soc. 42, 1937–1943.Google Scholar
Kreiner-Møller, M. & Stemmerik, L. (in press) Upper Permian lowstand fans of the Bredehorn Member, Schuchert Dal Formation, East Greenland. In: Sedimentary Environments Offshore Norway – Palaeozoic to Recent (Martinsen, O. & Dreyer, T., editors). Norwegian Petroleum Society, Special Publication. Elsevier, Amsterdam.Google Scholar
Lindgreen, H. (1991) Elemental and structural changes in illite/smectite mixed-layer minerals during diagenesis in Kimmeridgian-Volgian (-Ryazanian) clays in the Central Trough, North Sea and the Norwegi an-Danish Basin. Bull. Geol. Soc. Denmark. 39, 1–82.CrossRefGoogle Scholar
Mehra, O. & Jackson, M.L. (1960) Iron oxide removal from soils and clays by a dithionite-citrate system buffered with sodium bicarbonate. Clays Clay Miner. 7, 317–327.Google Scholar
Millot, G. (1970) Geology of Clays. Springer Verlag, London.Google Scholar
Milne, I.H. & Earley, J.W. (1958) Effect of source and environment on clay minerals. Am. Ass. Petrol. Geol. Bull. 42, 328–338.Google Scholar
Morgan, D.J. (1977) Simultaneous DTA-EGA of minerals and natural mineral mixtures. J. Therm. Anal. 12, 245–263.Google Scholar
Oberhänsli, H., Hsü, K.J., Piasecki, S. & Weissert, H. (1989) Permian-Triassic Carbon isotope anomaly in Greenland and in the Southern Alps. Historical Biol. 2, 37–49.Google Scholar
Pearson, M.J. & Small, J.S. (1988) Illite-smectite diagenesis and palaeotemperatures in northern North Sea Quaternary to Mesozoic shale sequences. Clay Miner. 23, 109–132.Google Scholar
Perry, E.A. & Hower, J. (1970) Burial diagenesis in Gulf Coast pelitic sediments. Clays Clay Miner. 18, 165–177.Google Scholar
Piasecki, S. & Marcussen, C. (1986) Oil geological studies in central East Greenland. Rep. Grønlands geol. Unders. 130, 95–102.Google Scholar
Reynolds, R.C. (1980) Interstratified clay minerals. Pp. 249–404 in: Crystal Structures of Clay Minerals and their X-ray Identification (Brindley, G.W. & Brown, G., editors). Monograph 5, Mineralogical Society, London.Google Scholar
Reynolds, R.C. & Hower, J. (1970) The nature of interlayering in mixed-layer illite-montmorillonite. Clays Clay Miner. 18, 25–36.Google Scholar
Surlyk, F. (1977) Mesozoic faulting in East Greenland. Geol. Mijnbouw. 56, 311–327.Google Scholar
Surlyk, F. (1978) Submarine fan sedimentation along fault scarps on tilted fault blocks (Jurassic– Cretaceous boundary, East Greenland). Bull. Grønlands geol. Unders. 128, 1–108.Google Scholar
Surlyk, F. (1987) Slope and deep shelf gully sandstones, Upper Jurassic, East Greenland. Am. Ass. Petrol. Geol. Bull., 464–475.Google Scholar
Surlyk, F. (1990) Timing, style and sedimentary evolution of Late Palaeozoic-Mesozoic extensional basins of East Greenland. Pp. 107–125 in: Tectonic Events Responsible for Britain's Oil and Gas Reserves (Hardman, R.F.P. & Brooks, J., editors). Special Publication, 55, Geological Society, London.Google Scholar
Surlyk, F. (1991) Sequence stratigraphy of the Jurassic-Lowermost Cretaceous of East Greenland. Am. Ass. Petrol. Geol. Bull. 75, 1468–1488.Google Scholar
Surlyk, F. & Noe-Nygaard, N. (1991) Sand bank and dune facies architecture of a wide intracratonic seaway: Late Jurassic-Early Cretaceous Raukelv Formation, Jameson Land, East Greenland. Pp. 261–276 in: The Three Dimensional Facies Architecture of Terrigenous Clastic Sediments and its Implications for Hydrocarbon Discovery and Recovery (Miall, A.D. & Tyler, N., editors). Society for Sedimentary Geology, Concepts and Models Series, 3.Google Scholar
Surlyk, F. & Noe-Nygaard, N. (2000) Shelf edge deltas, slope gullies and base-of-slope massive sands, Upper Jurassic, East Greenland: field analog for a complex type reservoir. 2000 AAPG Annual Convention, New Orleans, Louisiana, Official Programme, 9, A144.Google Scholar
Surlyk, F. & Noe-Nygaard, N. (in press) Cretaceous faulting and associated coarse-grained marine gravity-flow sedimentation, Traill Ì, East Greenland. In: Sedimentary Environments Offshore Norway – Palaeozoic to Recent (Martinsen, O.J. & Dreyer, T., editors). Norwegian Petroleum Society, Special Publication, Elsevier, Amsterdam.Google Scholar
Surlyk, F., Hurst, J.M., Piasecki, S., Rolle, F., Scholle, P.A., Stemmerik, L. & Thomsen, E. (1986) The Permian of the western margin of the Greenland Sea – A future explorat ion target. Pp. 629-659 in: Future Petroleum Provinces of the World (Halbouty, M.T., editor). Am. Ass. Petrol. Geol. Mem. 40.Google Scholar
van der Merwe, C.R. & Weber, H.W. (1963) The clay minerals of South African soils developed from granite under different climatic conditions. S. Afr. J. Agric. Sci. 6, 411–454.Google Scholar
Weaver, C.E. (1959) The clay petrology of sediments. Clays Clay Miner. 14, 154–187.Google Scholar
Weaver, C.E. & Beck, K.C. (1971) Clay water diagenesis during burial: how mud becomes gneiss. Geol. Soc. Am. Spec. Pap. 134, 1–78.Google Scholar
Wignall, P.B. & Ruffell, A.H. (1990) The influence of a sudden climatic change on marine deposition in the Kimmeridgian of North West Europe. J. Geol. Soc. 147, 365–372.Google Scholar
Wilson, M.J. (1971) Clay mineralogy of the Old Red Sandstone (Devonian) of Scotland. J. Sed. Pet. 41, 995–1007.Google Scholar