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Incremental pluton emplacement by magmatic crack-seal

Published online by Cambridge University Press:  11 January 2017

John M. Bartley ,
Drew S. Coleman  and
Allen F. Glazner
John M. Bartley
Affiliation:
Department of Geology and Geophysics, University of Utah, Salt Lake City, UT 84112-0111, USA, e-mail: bartley@earth.utah.edu
Drew S. Coleman
Affiliation:
Department of Geological Sciences, University of North Carolina, Chapel Hill, NC 27599, USA, e-mail: bartley@earth.utah.edu
Allen F. Glazner
Affiliation:
Department of Geological Sciences, University of North Carolina, Chapel Hill, NC 27599, USA, e-mail: bartley@earth.utah.edu
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Abstract

A growing body of evidence indicates that some, and perhaps most, plutons are highly composite. However, the geometrical forms of increments and the processes by which they are added are poorly known. Magmatic crack-seal probably is an important incremental assembly process, particularly in the upper crust where wall-rock fracture is important. Evidence for magmatic crack-seal is clearest where it is antitaxial, i.e., new fractures form at the contact between wall rock and a growing intrusion. Local deviation of antitaxial cracks into wall rocks isolates wall-rock bodies that therefore mark increment contacts. Wall rock isolated by this process remains in situ and thus is likely to preserve a ghost stratigraphy. Previously described plutons are identified, and interpreted to have grown by antitaxial magmatic crack-seal. In contrast, it remains unclear what observable geological record may remain in plutons formed by syntaxial crack-seal, in which new cracks form in the middle of the growing pluton. Several plutons are identified that preserve possible indirect evidence for growth by syntaxial crack seal, but conclusive identification of a direct record of the process remains elusive. However, plutons with sharp discordant contacts but few xenoliths may have been emplaced incrementally by syntaxial magmatic crack-seal.

Keywords

graniteincremental growthintrusive mechanism
Type
Research Article
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 97 , Issue 4 , 2008 , pp. 383 - 396
Copyright
Copyright © The Royal Society of Edinburgh 2008

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References

Annen, C., Scaillet, B. & Sparks, R.S.J. 2006. Thermal constraints on the emplacement rate of a large intrusive complex: The Manaslu Leucogranite, Nepal Himalaya. Journal of Petrology 47, 71-95.Google Scholar
Ague, J.J. & Brimhall, G.H. 1988. Magmatic arc asymmetry and distribution of anomalous plutonie belts in the batholiths of California; effects of assimilation, crustal thickness, and depth of crystallization. Geological Society of America Bulletin 100, 912-27.Google Scholar
Baker, A.A., Calkins, F.C., Crittenden, M.D. Jr. & Bromfield, C. S. 1966. Geologic map of the Brighton Quadrangle, Utah. U.S. Geological Survey GQ-534, 1:24,000.Google Scholar
Bartley, J.M., Wohletz, K., Coleman, D.S. & Glazner, A. F. 2004. Thermal modeling of large composite plutons. Eos, Transactions American Geophysical Union 85, 1935.Google Scholar
Bateman, P.C. 1992. Plutonism in the central part of the Siena Nevada batholith, California. U.S. Geological Survey Professional Paper 1483 Google Scholar
Bateman, P.C. & Chappell, B.W. 1979. Crystallization, fractionation. and solidification of the Tuolumne Intrusive Series, Yosemite National Park, California. Geological Society of America Bulletin 90, 465-82.Google Scholar
Bilodeau, B.J. & Nelson, C.A. 1993, Geology of the Sage Hen Flat pluton, White Mountains, California. Geological Society of America Map and Chart Series MCH077, 1:24,000.Google Scholar
Blake, D.H., Elwell, R.W.D., Gibson, I.L., Skelhorn, R.R. & Walker, G.P.L. 1965. Some relationships resulting from the intimate association of acid and basic magmas. Quarterly Journal of the Geological Society, London 121, 31-49.Google Scholar
Boudreau, A.E. & McBirney, A.R. 1997. The Skaergaard layered series; Part III, Non-dynamic layering. Journal of Petroloņv 38, 1003-20.Google Scholar
Brown, E.H. & McClelland, W.C. 2000. Pluton emplacement by sheeting and vertical ballooning in part of the southeast Coast Plutonic Complex, British Columbia. Geological Society of America Bulletin 112, 708-19.Google Scholar
Carl, B.S. & Glazner, A.F. 2002. Extent and significance of the Independence dike swarm, eastern California. Geological Society of America Memoir 195, 117-30.Google Scholar
Cobbing, E.J. 1999. The Coastal Batholith and other aspects of Andean magmatismi in Peru. In Castro, A., Fernandez, C., & Vigneresse, J.L. (eds) Understanding Granites: Integrating New and Classical Techniques, 111-22. London: Geological Society Special Publication.Google Scholar
Coleman, D.S., Glazner, A.F., Miller, J.S., Bradford, K.J., Frost, T.P., Joye, J.L. & Bachi, C.A. 1995. Exposure of a Late Cretaceous layered mafic-felsic magma system in the central Sierra Nevada batholith, California. Contributions to Mineralogy and Petrology 120, 129-36.Google Scholar
Coleman, D.S., Gray, W. & Glazner, A.F. 2004. Rethinking the Emplacement and Evolution of Zoned Plutons: Geochronologie Evidence for Incremental Assembly of the Tuolumne Intrusive Suite, California. Geology 32, 433-6.Google Scholar
Coleman, D.S., Bartley, J.M., Glazner, A.F. & Law, R.D. 2005. Incremental Assembly and Emplacement of Mesozoic Plutons in the Sierra Nevada and White and Inyo Ranges, California: Geological Society of America Field Forum Field Trip Guide, doi: 10.1130/2005. MCBFYT.FFG.Google Scholar
Condon, D.J., Bowring, S.A., Pitcher, W.S. & Hutton, D.W.H. 2004. Rates and tempo of granitic magmatism; a U-Pb geo-chronological investigation of the Donegal Batholith (Ireland). Geological Society of’America Abstracts with Programs 36, 5, 406.Google Scholar
Constenius, K.N. 1996. Extensional tectonics of the Cordilleran foreland fold and thrust helt and the Jurassic-cretaceous Great Valley forcare basin, Ph.D. Dissertation. University of Arizona, Tucson.Google Scholar
Crittenden, M.D. 1965. Geology of the Dromedary Peak quadrangle, Utah. U.S. Geological Survey Map GQ-378, 1:24,000.Google Scholar
Cruden, A. R. Grocott, J., McCaffrey, K.J.W. & Davis, D.D. 2005. Timescales of incremental pluton growth; theory and a field-based test. Geological Society of America Abstracts with Programs 37, 7, 131.Google Scholar
Cruden, A.R. & McCaffrey, K.J.W. 2001. Growth of plutons by floor subsidence; implications for rates of emplacement, intrusion spacing and melt-extraction mechanisms. Physics and Chemistry of the Earth. Part A: Solid Earth and Geodesy 26, 303-15.Google Scholar
Didericksen, B. & Bartley, J.M. 2003. Did kilometer-scale flow of interstitial melt erase evidence of incremental emplacement of the Alta Stock? Geological Society of America Abstracts With Programs 35, 7, 181.Google Scholar
Flinders, J. & Clemens, J.D. 1996. Non-linear dynamics, chaos, complexity and enclaves in granitoid magma. Transactions of the Royal Society of Edinburgh: Earth Sciences 87, 217-23.Google Scholar
Frost, T.P. & Mahood, G.A. 1987. Field, chemical, and physical constraints on mafic-felsic magma interaction in the Lamarck Granodiorite, Sierra Nevada, California. Geological Society of America Bulletin 99, 272-91.Google Scholar
Cierbi, C., Johnson, S.E. & Paterson, S.R. 2004. Implications of rapid, dike-fed pluton growth for host-rock strain rates and emplacement mechanisms. Journal of Structural Geology 26, 583-94.Google Scholar
Glazner, A.F., Bartley, J.M., Coleman, D.S., Gray, W.M. & Taylor, R.Z. 2004. Are plutons assembled over millions of years by amalgamation from small magma chambers? Geological Society of America Today 14, 4/5, 4-11.Google Scholar
Glazner, A.F., Carl, B.S., Coleman, D.S., Miller, J.S. & Bartley, J.M. 2008. Chemical variability and composite nature of dikes from the Late Jurassic Independence dike swarm, eastern California. In Shervais, J.W. & Wright, J.E. (eds) Arcs, Ophiolites. and Batholiths: A Tribute to Cliff Hopson. Geological Society of America Special Paper 438, 455-80. doi:10.1130/2008.2438(16).Google Scholar
Glazner, A.F. & Bartley, J.M. 2006. Is stoping a volumetrically significant pluton emplacement process? Geological Society of America Bulletin 118, 1185-95.Google Scholar
Glazner, A.F. & Miller, D.M. 1997. Late-stage sinking of plutons. Geology 25, 1099-102.Google Scholar
Gray, W.M. 2003. Chemical and thermal evolution of the Late Cretaceous Tuolumne Intrusive Suite, Yosemite National Park, California, Ph.D. Dissertation. University of North Carolina, Chapel Hill.Google Scholar
Hamilton, W. & Myers, W.B. 1967. The nature of batholiths. U.S. Geological Survey, Professional Paper 554-C. Google Scholar
Hanson, R.B. & Glazner, A.F. 1995. Thermal requirements for extensional emplacement of granitoids. Geology 23, 213-16.Google Scholar
John, D.A. 1989. Geologic setting, depths of emplacement, and regional distribution of fluid inclusions in intrusions of the central Wasatch Mountains, Utah. Economic Geology 84, 386-409.Google Scholar
Jowhar, T.N. 2001. Geobarometric constraints on the depth of emplacement of granite from the Ladakh Batholith, Northwest Himalaya, India. Journal of Mineralogical and Petrological Sciences 96, 256-64.Google Scholar
Leake, B.E. & Cobbing, J. 1993. Transient and long-term correspondence of erosion level and the tops of granite plutons. Scottish Journal of Geology 29, 177-82.Google Scholar
Mahan, K.H., Bartley, J.M., Coleman, D.S., Glazner, A.F. & Carl, B. S. 2003. Sheeted intrusion of the synkinematic McDoogle pluton, Sierra Nevada, California. Geological Society of America Bulletin 115, 1570-82.Google Scholar
Marsh, B.D. 1982. On the mechanics of igneous diapirism, stoping, and zone melting. American Journal of Science 282, 808-55.Google Scholar
Matzel, J., Mundil, R., Paterson, S., Renne, P. & Nomade, S. 2005. Evaluating pluton growth models using high resolution geochronology: Tuolumne Intrusive Suite, Sierra Nevada, CA. Geological Society of America Abstracts with Programs 37, 7, 131.Google Scholar
Matzel, J.E.P., Bowring, S.A. & Miller, R.B. 2006. Time scales of pluton construction at differing crustal levels; examples from the Mount Stuart and Tenpeak Intrusions, north Cascades, Washington. Geological Society of America Bulletin 118, 1412-30.Google Scholar
McBirney, A.R. & Hunter, R.H. 1995. The cumulate paradigm reconsidered. Journal of Geology 103, 114-22.CrossRefGoogle Scholar
Metcalf, R.V., Smith, E.I., Walker, J.D., Reed, R.C., Gonzales, D. A. 1995. Isotopie disequilibrium among commingled hybrid magmas; evidence for a two-stage magma mixing-commingling process in the Mt. Perkins Pluton, Arizona. Journal of Geology 103, 509-27.Google Scholar
Miller, C. F., Watson, E.B. & Harrison, T.M. 1988. Perspectives on the source, segregation and transport of granitoid magmas. Transactions of the Royal Society of Edinburgh: Earth Sciences 79, 135-56.Google Scholar
Miller, C. F. & Miller, J.S. 2002. Contrasting stratified plutons exposed in tilt blocks, Eldorado Mountains, Colorado River Rift, NV, USA. Lithos 61, 209-24.Google Scholar
Moore, J.G. 1963. Geology of the Mount Pinchot Quadrangle, southern Sierra Nevada, California. U.S. Geological Survey Bulletin 1130, 1-152.Google Scholar
Moore, J.G. & Hopson, C.A. 1961. The Independence dike swarm in eastern California. American Journal of Science 259, 241-59.Google Scholar
Morgan, S.S., Law, R.D. & Saint Blanquat, M. 2000. Papoose Flat, EJB and Sage Hen Flat plutons: Examples of rising, sinking and cookie-cutter plutons in the White-Inyo Range, eastern California. In Lageson, D.R., Peters, S.G. & Lahren, M. (eds) Great Basin and Sierra Nevada. Geological Society of America Field Guide 2, 189-204.CrossRefGoogle Scholar
Boulder, Colorado, Nelson, C.A. 1971. Geologic map of the Waucoba Spring quadrangle, Inyo County, California. U.S. Geological Survey GQ-921, 1:62,500.Google Scholar
Paterson, S. R. 1998. Late-stage sinking of plutons-Comment. Geology 26, 863.Google Scholar
Paterson, S.R., Yuan, E.S., Miller, R.B. & Pitcher, W.S. 1994. Emplacement of the main Donegal Granite, Ireland. Geological Society of America Abstracts with Programs 26, 2, 80.Google Scholar
Paterson, S.R. & Fowler, T.K. Jr., 1993. Re-examining pluton emplacement processes. Journal of Structural Geology 15, 191-206.Google Scholar
Paterson, S.R. & Tobisch, O.T. 1992. Rates of processes in magmatic arcs; implications for the timing and nature of pluton emplacement and wall rock deformation. Journal of Structural Geology 14, 291-300.Google Scholar
Petford, N. 1996. Dykes or diapirs. Transactions of the Royal Society of Edinburgh: Earth Sciences 87, 105-14.Google Scholar
Petford, N., Cruden, A.R., McCaffrey, K.J.W. & Vigneresse, J.-L. 2000. Granite magma formation, transport, and emplacement in the Earth’s crust. Nature 408, 669-73.Google Scholar
Petford, N. & Koenders, M.A. 2003. Shear-induced pressure changes and seepage phenomena in a deforming porous layer I. Geophysical Journal International 155, 857-69.CrossRefGoogle Scholar
Pitcher, W.S. 1979. The nature, ascent, and emplacement of granitic magmas. Journal of the Geological Society, London 136, 627-62.Google Scholar
Pitcher, W.S. 1993. The Nature and Origin of Granite. London: Chapman & Hall.Google Scholar
Pitcher, W.S. & Berger, A.R. 1972. The Geology of Donegal: A Study of Granite Emplacement and Unroofing. New York: Wiley Interscience.Google Scholar
Pitcher, W.S. & Hutton, D.H.W. 2003. A Master Class Guide to the Granites of Donegal. Dublin, Ireland: Geological Survey of Ireland.Google Scholar
Ramsay, J.G. 1980a. The crack-seal mechanism of rock deformation. Nature 284, 135-9.Google Scholar
Ramsay, J.G. 1908b. Shear zone geometry; a review. Journal of Structural Geology 2, 83-99.Google Scholar
Sibson, R.H. 1982. Fault zone models, heat flow, and the depth distribution of earthquakes in the continental crust of the United States. Bulletin of the Seismological Society of America 72, 151-63.Google Scholar
Sisson, T.W., Grove, T.L. & Coleman, D.S. 1996. Hornblende gabbro sili complex at Onion Valley, California, and a mixing origin for the Sierra Nevada batholith. Contributions to Mineralogy and Petrology 126, 81-108.Google Scholar
Sleep, N. H. 1975. Formation of oceanic crust: some thermal constraints. Journal of Geophysical Research 80, 4037-12.Google Scholar
Snyder, D. & Tait, S. 1995. Replenishment of magma chambers: comparison of fluid-mechanic experiments with field relations. Contributions to Mineralogy and Petrology 122, 230-40.Google Scholar
Snyder, D. & Tait, S. 1998. A flow-front instability in viscous gravity currents. Journal of Fluid Mechanics 369, 1-21.Google Scholar
Taylor, R.Z. 2004. Structure and petrology of an interpluton screen at May Lake, Yosemite National Park, California, M.S. Thesis. University of North Carolina, Chapel Hill.Google Scholar
Tikoff, B. & Teyssier, C. 1992. Crustal-scale, en echelon ‘P-shear’ tensional bridges: A possible solution to the batholithic room problem. Geology 20, 927-30.Google Scholar
Vogel, T. A., Cambray, F. W., Feher, L., Constenius, K. N., Copeland, P.C., Flood, T.P., Garzione, C., Geherels, G.E., Hodkinson, D., Hanson, S.L., Hoist, T.B., John, D.A. & Layer, P. W. 1997. Petrochemistry and emplacement history of the Wasatch igneous belt. Guidebook Series - Society of Economic Geologisis 29, 35-16.Google Scholar
Vogel, T.A., Cambray, F.W. & Constenius, K. N. 2001. Origin and emplacement of igneous rocks in the central Wasatch Mountains, Utah. Rocky Mountain Geology 36, 119-62.Google Scholar
Wager, L. R. & Brown, G. M. 1968. Layered Igneous Rocks. Edinburgh: Oliver and Boyd.Google Scholar
Walker, B.A., Miller, C. F., George, B.E., Ludington, S., Wooden, J. L., Bleick, H.A. & Miller, J.S. 2005. The Spirit Mountain Batholith: Documenting Magma Storage in the Upper Crust One Pulse at a Time. Eos, Transactions of the American Geophysical Union 86, V21A-03Google Scholar
Walker, D., Jurewicz, S. & Watson, E.B. 1988. Adcumulus dunite growth in a laboratory thermal gradient. Contributions to Mineralogy and Petrology 99, 306-19.Google Scholar
Wiebe, R.A. 1993. The Pleasant Bay layered gabbro-diorite, coastal Maine; ponding and crystallization of basaltic injections into a silicic magma chamber. Journal of Petrology 34, 461-89.Google Scholar
Wiebe, R.A. 1994. Silicic magma chambers as traps for basaltic magmas: the Cadillac Mountain intrusive complex, Mount Desert Island, Maine. Journal of Geology 102, 423-37.Google Scholar
Wiebe, R.A., Blair, K. D., Hawkins, D.P. & Sabine, C.P. 2002. Mafic injections, in situ hybridization, and crystal accumulation in the Pyramid Peak granite, California. Geological Society of America Bulletin 114, 909-20.2.0.CO;2>CrossRefGoogle Scholar
Wiebe, R. A. & Collins, W.J. 1998. Depositional features and stratigraphie sections in granitic plutons; implications for the emplacement and crystallization of granitic magma. Journal of Structural Geology 20, 1273-89.Google Scholar
Wilson, J. C. 1961. Geology of the Alta Stock, Utah, Ph.D. Dissertation. California Institute of Technology, Pasadena.Google Scholar
Wohletz, K. H. & Heiken, G. 1992. Voleanology and Geothermal Energy. Berkeley, CA: University of California Press.Google Scholar
Yoshinobu, A.S., Okaya, D.A. & Paterson, S.R. 1998. Modeling the thermal evolution of fault-controlled magma emplacement models; implications for the solidification of granitoid plutons. Journal of Structural Geology 20, 1205-18.Google Scholar
Yoshinobu, A.S., Fowler, T.K. Jr., Paterson, S.R., Llambias, E., Tickyj, H. & Sato, A.M. 2003. A view from the roof; magmatic stoping in the shallow crust, Chita Pluton, Argentina. Journal of Structural Geology 25, 1037-48.Google Scholar