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The exhumation history of orogenic belts from 40Ar/39Ar ages of detrital micas

Published online by Cambridge University Press:  05 July 2018

F. M. Stuart
F. M. Stuart*
Affiliation:
Isotope Geosciences Unit, Scottish Universities Environmental Research Centre, East Kilbride G75 0QF, UK
*
*E-mail: [email protected]
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Abstract

The exhumation history of mountain belts can be derived from radiometric dating of detrital mineral grains in proximal and distal post- and synorogenic sediments. The application of single-crystal dating techniques avoids the averaging effect that characterizes multi-grain and whole-rock techniques and allows the identification of populations of grains with distinct thermal histories. Of the major single crystal dating methods available, 40Ar/39Ar dating of detrital K-bearing minerals, in particular white mica, is perhaps the most versatile and widely applied technique. For a closure temperature of Ar of 350–400°C, muscovite 40Ar/39Ar ages record the time a rock mass passed through 8–10 km beneath actively eroding mountain belts. Detrital muscovit ages eroded from orogenic mountain belts have been used extensively to identify the provenance of sediments from source regions with distinct thermal histories, determine the history and rate of exhumation of the source region, and provide an upper limit on the sediment age. Here I review the principles of 40Ar/39Ar dating of detrital muscovite and illustrate the method with examples showing how the provenance and the thermal history of sediment source regions derived from such studies can be used to constrain the exhumation and tectonic history of orogenic belts.

Keywords

Ar/Armuscoviteerosiondepositionprovenance
Type
Research Article
Information
Mineralogical Magazine , Volume 66 , Issue 1 , February 2002 , pp. 121 - 135
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2002

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References

Aalto, K.R., Sharp, W.D. and Renne, P.R. (1998) 40Ar/39Ar dating of detrital mics from Oligocene-Pleistocene sandstones of the Olympic Peninsula, Klamath Mountains, and northern California Coast Ranges: Provenenance and palaeodrainage patterns. Canadian Journal of Earth Science, 35, 735–745.CrossRefGoogle Scholar
Andersen, T.B, Jamtviet, B., Dewey, J.F. and Swensson, E. (1991) Subduction and eduction of continental crust: major mechanisms during continent-continent collision and orogenic extension, a model based on the S. Norway Caledonides. Terra Research, 3, 303–310.Google Scholar
Andersen, T.B, Berry, H.N., Lux, D.R. and Andresen, A. (1998) Tectonic significance of pre-Scandian 40Ar/39Ar cooling ages in the Caledonides of western Norway. Journal of the Geological Society of London, 155, 297–309.CrossRefGoogle Scholar
Boundy, T.M., Essene, E.J., Hall, C.M., Austrheim, A. and Halliday, A. (1996) Rapid exhumation of lower crust during continent collision and late extension: Evidence from 40Ar/39Ar incremental heating of hornblendes and muscovites, western Norway. Geological Society of America Bulletin, 108, 1425–1437.2.3.CO;2>CrossRefGoogle Scholar
Brandon, M.T. and Vance, J.A. (1992) New statistical methods for the analysis of fission track grain-age distributions with applications to detrital zircon ages from the Olympic subduction complex, western Washington State. American Journal of Science, 292, 985–1009.CrossRefGoogle Scholar
Carter, A. (1999) Present status and future avenues of source region discrimination and characterization using fission track analysis. Sedimentary Geology, 124, 31–45.CrossRefGoogle Scholar
Carter, A. and Moss, SJ. (1999) Combined detrital-zircon fission-track and U-Pb dating: A new approach to understanding hinterland evolution. Geology, 27, 235–238.2.3.CO;2>CrossRefGoogle Scholar
Chauvet, A. and Dallmeyer, R.D. (1992) 40Ar/39Ar mineral dates related to Devonian extension in the southwestern Scandinavian Caledonides. Tectonophysics, 210, 155–177.CrossRefGoogle Scholar
Clauer, N. (1981) Strontium and argon isotopes in naturally weathered biotites, muscovites and feldspars. Chemical Geology, 31, 325–334.CrossRefGoogle Scholar
Cliff, R.A, Drewery, S.E. and Leeder, M.R. (1991) Sourcelands for the Carboniferous Pennine River system: constraints from sedimentary evidence and U-Pb geochronology using zircon and monazite. Pp. 137–159 in: Developments in Sedimentary Provenance Studie. (Morton, A.C., Todd, S.P. and Haughton, P.D.W., editors). Special Publication, 57. Geological Society, London.Google Scholar
Cohen, H.A, Hall, C.M. and Lundberg, N. (1995) 40Ar/39Ar dating of detrital grains constrain the provenance and stratigraphy of the Gravina belt, Southeastern Alaska. Journal of Geology, 103, 327–337.CrossRefGoogle Scholar
Coker, J.E., Steltenpohl, M.G., Andresen, A. and Kunk, M. (1995) An 40Ar/39Ar thermochronology of the Ofoten-Troms region: Implications for terrane amalgamation and extensional collapse of the northern Scandinavian Caledonides. Tectonics, 14, 435–447.CrossRefGoogle Scholar
Copeland, P. and Harrison, T.M. (1990) Episodic rapid uplift in the Himalaya revealed by 40Ar/39Ar analysis of detrital K-feldpsar and muscovite, Bengal fan. Geology, 18, 354–357.2.3.CO;2>CrossRefGoogle Scholar
Copeland, P., Harrison, T.M., Hodges, K.V., Maruejol, P., LeFort, P. and Pecher, A. (1991) An early Eocene thermal disturbance of the Main Central Thrust, central Nepal: implications for Himalayan tectonics. Journal of Geophysical Research, 96, 8475–8500.CrossRefGoogle Scholar
Corrigan, J.D. and Crowley, K.D. (1990) Fission-track analysis of detrital apatites from ODP sites 717 and 718, leg 116, central Indian Ocean. Proceedings of the Ocean Drilling Program, Scientific Results, 116, 75–92.Google Scholar
Craw, D., Koons, P.O., Winslow, D., Chamberlain, C.P. and Zeitler, P. (1994) Boiling fluids in a region of rapid uplift, Nanga Parbat, Pakistan. Earth and Planetary Science Letters, 128, 169–182.CrossRefGoogle Scholar
Dallmeyer, R.D. (1987) 40Ar/39Ar age of detrital muscovite within lower Ordovician sandstone in the coastal plain basement of Florida: Implications for west Africa terrane linkage. Geology, 15, 9981–001.2.0.CO;2>CrossRefGoogle Scholar
Dallmeyer, R.D. (1988) Polyorogenic 40Ar/39Ar mineral age record within the Kalak Nappe Complex, Northern Scandinavian Caledonides. Journal of the Geological Society of London, 145, 705–716.CrossRefGoogle Scholar
Dallmeyer, R.D. (1990) 40Ar/39Ar mineral age record of a polyorogenic evolution within the Seve and Koli nappes, Trondelag, Norway. Tectonophysics, 179, 199–226.CrossRefGoogle Scholar
Dallmeyer, R.D. and Andresen, A. (1992) Polyphase tectonothermal evolution of exotic Caledonian nappes in Troms, Norway: Evidence from 40Ar/39Ar mineral age. Lithos, 29, 19–42.CrossRefGoogle Scholar
Dallmeyer, R.D. and Gee, D.G. (1986) 40Ar/39Ar mineral dates from retrogressed eclogites within the Baltoscandian miogeocline: Implications for a polyphase Caledonian orogenic evolution. Geological Society of America Bulletin, 97, 26–34.2.0.CO;2>CrossRefGoogle Scholar
Dallmeyer, R.D. and Gee, D.G. (1987) Polyorogenic 40Ar/39Ar age record of the Seve and Koli nappes of the Gaddede area, northwestern Jamtland, central Scandinavia. Journal of Geology, 96, 181–198.CrossRefGoogle Scholar
Dallmeyer, R.D. and Gee, D.G. (1989) Polyorogenic 40Ar/39Ar age record of the Seve and Koli nappes of the Gaddede area, northwestern Jamtland, central Scandinavia. Journal of Geology, 96, 181–198.CrossRefGoogle Scholar
Dallmeyer, R.D., Gee, D. and Beckholmen, M. (1985) 40Ar/39Ar mineral age record of early Caledonian tectonothermal activity in the Baltoscandian miogeo-cline. American Journal of Science, 285, 532–568.CrossRefGoogle Scholar
Dallmeyer, R.D., Johansson, L. and Moller, C. (1992) Chronology of Caledonian high-pressure granulite-facies metamorphism, uplift and deformation within northern parts of the Western Gneiss Region Norway. Geological Society of America Bulletin, 104, 444–455.2.3.CO;2>CrossRefGoogle Scholar
Dallmeyer, R.D., Strachan, R.A. and Henriksen, N. (1994) 40Ar/39Ar mineral age record in NE Greenland: implications for tectonic evolution of the North Atlantic Caledonides. Journal of the Geological Society of London, 151, 615–628.CrossRefGoogle Scholar
Damon, P.E. and Kulp, J.L. (1958) Excess helium and argon in beryl and other minerals. American Mineralogist, 43, 433–459.Google Scholar
Deino, A. and Potts, R. (1989) Age-probability spectra for examination of single-crystal 40Ar/39Ar dating results: Examples from Olorgesaille, Southern Kenya Rift. Quaternary International, 13/14, 47–53.Google Scholar
Dodson, M.H. (1973) Closure temperature in cooling geochronological and petrological systems. Contributions to Mineralogy and Petrology, 40, 259–274.CrossRefGoogle Scholar
Dunlap, W.J. and Fossen, H. (1998) Early Palaeozoic collapse, tectonic stability, and late Palaeozoic continental rifting revealed through thermochronology of K-feldspars from South Norway. Tectonics, 17, 604–620.CrossRefGoogle Scholar
Eide, E.A, Torsvik, T.H., Andersen, T.B. and Arnaud, N.O. (1999) Early Carboniferous unroofing in western Norway: A tale of alkali feldspar thermochronology. Journal of Geology, 107, 353–374.CrossRefGoogle Scholar
Fossen, H. and Dunlap, W.J. (1998) Timing and kinematics of Caledonian thrusting and extensional collapse, S. Norway: Evidence from 40Ar/39Ar thermochronology. Journal of Structural Geology, 20, 765–781.CrossRefGoogle Scholar
Garver, J.I., Brandon, M.T., Roden-Tice, M. and Kamp, P.J. (1999) Exhumation history of orogenic high-lands determined by detrital fission-track thermochronology. Pp. 283–304 in: Exhumation Processes: Normal Faulting, Ductile Flow and Erosion (Ring, U., Brandon, M.T., Lister, G.S. and Willett, S.D., editors). Special Publication, 154. Geological Society, London.Google Scholar
Hallsworth, C.R., Morton, A.C, Claoue-Long, J. and Fanning, C.M. (2000) Carboniferous sand provenance in the Pennine Basin, UK: Constraints from heavy mineral and detrital zircon age data Sedimentary Geology, 137, 147–185.CrossRefGoogle Scholar
Hames, W.E. and Andresen, A. (1996) Timing of Palaeozoic orogeny and extension in the continental shelf of north-central Norway as indicated by laser 40Ar/39Ar muscovite dating. Geology, 24, 1005–1008.2.3.CO;2>CrossRefGoogle Scholar
Hames, W.E. and Bowring, S.A. (1994) An empirical evaluation of the argon diffusion geometry in muscovite. Earth and Planetary Science Letters, 124, 161–167.CrossRefGoogle Scholar
Heller, P.L, Petermen, Z.E., O’Neil, J.R. and Shafiqullah, M. (1985) Isotopic provenance of sadstones from the Eocene Tyree Formation, Oregon Coast Range. Geological Society of America Bulletin, 96, 770–780.2.0.CO;2>CrossRefGoogle Scholar
Heller, P.L., Renne, P.R. and O’Neil, J.R. (1992) River mixing rate, residence time and subsidence rates from isotopic indicators: Eocene sandstones of the U.S. Pacific Northwest. Geology, 20, 1095–1098.2.3.CO;2>CrossRefGoogle Scholar
Hodges, K.V., Hames, W.E. and Bowring, S.A. (1994) 40Ar/39Ar age gradients in micas from a high temperature- low pressure metamorphic terrain: Evidence for very slow cooling and implications for the interpretation of age spectra. Geology, 22, 55–58.2.3.CO;2>CrossRefGoogle Scholar
House, M.A, Farley, K.A. and Stockli, D. (2000) Helium chronometry of apatite and titanite using Nd-YAG laser heating. Earth and Planetary Science Letters, 183, 365–368.CrossRefGoogle Scholar
Kelley, S.P. (1995) Ar-Ar dating by laser microprobe. Pp. 327–358 in: Microprobe Techniques in the Earth Science. (Potts, P.J., Bowles, J.F.W., Reed, S.J.B. and Cave, M.R., editors). Mineralogical Society Series, 6. Chapman & Hall, London.CrossRefGoogle Scholar
Kelley, S.P. and Bluck, B.J. (1989) Detrital mica ages from the Southern Uplands using 40Ar/39Ar laser probe. Journal of the Geological Society of London, 146, 401–403.CrossRefGoogle Scholar
Kelley, S.P. and Bluck, B.J. (1992) Laser 40Ar/39Ar ages for individual detrital muscovites in the Southern Uplands of Scotland, UK. Chemical Geology (Isotope Geoscience Section), 101, 143–156.CrossRefGoogle Scholar
Laslett, G.M. and Galbraith, R.F. (1996) Statistical modelling of fission tracks in apatite. Geochimica et Cosmochimica Acta, 60, 5117–5131.CrossRefGoogle Scholar
Li, S., Wang, S., Chen, Y., Liu, D., Zhou, H. and Zhang, Z. (1994) Excess argon in phengite from eclogite: Evidence from dating of eclogite minerals by Sm-Nd, Rb-Sr and 40Ar/39Ar methods. Chemical Geology, 112, 343–350.CrossRefGoogle Scholar
Lister, G.S. and Baldwin, S.L. (1996) Modelling the effect of arbitrary P-T-t histories on argon diffusion in minerals using the MacArgon program for the Apple Macintosh. Tectonophysics, 253, 83–109.CrossRefGoogle Scholar
McDougall, I. and Harrison, T.M. (1999) Geochronology and Thermochronolo gy by the 40Ar/9Ar Method. Oxford University Press, UK, 269 pp.Google Scholar
Mancketlow, N.S. and Grasemann, B. (1997) Time-dependent effects of heat advection and topography on cooling histories during erosion. Tectonophysics, 270, 167–195.CrossRefGoogle Scholar
McCabe, P.J. (1977) Deep distributary channels and giant bedforms in the Upper Carboniferous of the Central Pennines, England. Sedimentology, 24, 271–290.CrossRefGoogle Scholar
Miller, R.G. and O’Nions, R.K. (1984) The provenance and crustal residence ages of British sediments in relation to palaeogeographic reconstructions. Earth and Planetary Science Letters, 68, 459–470.CrossRefGoogle Scholar
Monie, P. and Chopin, C. (1991) 40Ar/39Ar dating in coesite-bearing and associated units of the Doria Maitra massif, western Alps. European Journal of Mineralogy, 3, 239–262.CrossRefGoogle Scholar
Morton, A.C. and Hallsworth, C.R. (1999) Processes controlling the composition of heavy mineral assemblages in sandstones. Sedimentary Geology. 124, 3–29.CrossRefGoogle Scholar
Morton, A.C, Claoue-Long, J. and Berge, C. (1996) SHRIMP constraints on sediment provenance and transport history in the Mesozoic Stratfjord Formation. Journal of the Geological Society of London, 153, 915–923.CrossRefGoogle Scholar
Najman, Y., Pringle, M.S., Johnson, M.R.W., Robertson, A.H. and Wijbrans, J.R. (1997) Laser 40Ar/39Ar dating of single detrital muscovite grains from early foreland-basin sedimentary deposits in India: Implications for early Himalayan evolution. Geology, 25, 535–538.2.3.CO;2>CrossRefGoogle Scholar
Najman, Y., Pringle, M., Godin, L. and Oliver, G. (2001) Dating the oldest continental sediments from the Himalayan foreland basin. Nature, 410, 194–196.CrossRefGoogle ScholarPubMed
Northrup, C.J. (1997) Timing structural assembly, metamorphism and cooling of Caledonian nappes in the Ofoten-Efjorden Area, N. Norway: tectonic insights from U-Pb and 40Ar/39Ar geochronology. Journal of Geology, 105, 565–582.CrossRefGoogle Scholar
Parsons, I., Brown, W.L. and Smith, J.V. (1999) 40Ar/39Ar thermochronology using alkali feldspars: Real thermal history or mathematical mirage of microtexture? Contributions to Mineralogy and Petrology, 136, 92–110.CrossRefGoogle Scholar
Phillips, D. and Onstott, T.C. (1988) Argon isotope zoning in mantle phlogopite. Geology, 16, 542–546.2.3.CO;2>CrossRefGoogle Scholar
Reiners, P.W., Brady, R, Farley, K.A, Fryxell, J.E., Wernicke, B.P. and Lux, D. (2000) He and Ar thermochronology of the Gold Butte block, south Virgin Mountains, Nevada. Earth and Planetary Science Letters, 178, 315–326.CrossRefGoogle Scholar
Renne, P.R., Becker, T.A. and Swapp, S.M. (1990) 40Ar/39Ar laser-probe dating of detrital micas from the Montgomery Creek Formation, northern California: Clues to provenance, tectonics and weathering processes. Geology, 18, 563–566.2.3.CO;2>CrossRefGoogle Scholar
Roddick, J.C., Cliff, R.A. and Rex, D.C. (1980) The evolution of excess argon in alpine biotites – A 40Ar/39Ar analysis. Earth and Planetary Science Letters, 48, 185–208.CrossRefGoogle Scholar
Rohrman, R, Andriessen, P. and van der Beek, P. (1996) The relationship between basin and margin thermal evolution assessed by fission track thermochronology and application to offshore southern Norway. Basin Research, 8, 45–63.CrossRefGoogle Scholar
Sherlock, S.C. (2001) Two stage erosion and deposition in a continental margin setting: a 40Ar/39Ar laser-probe study of offshore detrital white micas in the Norwegian Sea. Journal of the Geological Society of London, 158, 793–799.CrossRefGoogle Scholar
Sherlock, S.C, Jones, K.A. and Jones, J.A. (2000) A central European Variscide source for Upper Carboniferous sediments in SW England: 40Ar/39Ar detrital white mica ages from the Forest of Dean Basin. Journal of the Geology Society of London, 157, 905–908.CrossRefGoogle Scholar
Sherlock, S.C, Jones, K.A. and Kelley, S.P. (in press) Fingerprinting polyorogenic detritus using the 40Ar/39Ar UV laserprobe. Geology. Google Scholar
Simpson, R.L., Parrish, R.R., Searle, M.P. and Waters, D.J. (2000) Two episodes of monazite crystallization during metamorphism and crustal melting in the Everest region of the Nepalese Himalaya. Geology, 28, 403–406.2.0.CO;2>CrossRefGoogle Scholar
Stuart, F.M., Bluck, B.J. and Pringle, M. (2001) 40Ar/39Ar ages of detrital muscovites from Upper Devonian-Carboniferous sandstones of northern UK: Provenance and implications for the history of orogenic belts. Tectonics, 20, 255–267.CrossRefGoogle Scholar
Suarez-Fernandez, J., Alonso-Gutierrez, G., Jenner, G.A. and Tubrett, M.N. (2000) New ideas on the Proterozoic–Early Palaeozoic evolution of the NW Iberia: Insights from U-Pb detrital zircon ages. Precambrian Research, 102, 185–206.CrossRefGoogle Scholar
Tagami, T., Galbraith, R.F., Yamada, G.M. and Laslett, G.M. (1998) Revised annealing kinetics of fission tracks in zircon and geological implications. Pp. 99–112 in: Advances in Fission Track Geochronolog. (Van den Haute, P. and De Corte, F., editors). Kluwer, Dordrecht, The Netherlands.CrossRefGoogle Scholar
Tilke, P.G. (1988) Caledonian structure, metamorphism. geochronology, and tectonics of the Sitas-Singas area, Sweden. PhD dissertation, Massachusetts Institute of Technology, Cambridge, MA, USA.Google Scholar
Treloar, P.J. and Searle, M.P. (editors) (1993) Himalayan Tectonics. Special Publication, 74. Geological Society of London, 630 pp.Google Scholar
Turner, S.P., Kelley, S.P., Vanden Berg, A.H., Foden, J.D., Sandiford, M. and Flottman, T. (1996) Source of the Lachlan fold belt flysch linked to convective removal of the lithospheric mantle and rapid exhumation of the Delamerian-Ross fold belt. Geology, 24, 941–944.2.3.CO;2>CrossRefGoogle Scholar
Von Eynatten, R, Gaupp, G. and Wijbrans, J.R. (1996) 40Ar/39Ar laser-probe dating of detrital white micas from Cretaceous sedimentary rocks of the Eastern Alps: Evidence for Variscan high-pressure metamorphism and implications for Alpine orogeny. Geology, 24, 691–694.2.3.CO;2>CrossRefGoogle Scholar
Von Eynatten, R, Schunlegger, F., Gaupp, G. and Wijbrans, J.R. (1999) Exhumation of the Central Alps: evidence from 40Ar/39Ar laserprobe dating of detrital white micas from the Swiss Molasse Basin. Terra Nova, 11, 284–289.CrossRefGoogle Scholar
Wagner, G.A, Miller, D.S. and Jager, E. (1979) Fission track ages on apatite of Bergell rocks from Central Alps and Bergell boulders in Oligocene sediments. Earth and Planetary Science Letters, 45, 355–360.CrossRefGoogle Scholar
White, N.M., Pringle, M., Garzanti, E., Najman, Y., Bickle, M., Friend, P., Maithani, A. and Burbank, D. (2000) Ar/Ar single crystal white mica ages for Himalayan erosion, exhumation and provenance studies. Goldschmidt Conference abstract, Cambridge Publications, 1083.Google Scholar
Wijbrans, J.R. and McDougaU, I. (1986) 40Ar/39Ar dating of white micas from an Alpine high-pressure metamorphic belt on Naxos (Greece): The resetting of the argon isotopic system. Contributions to Mineralogy and Petrology, 93, 187–194.CrossRefGoogle Scholar
Williams, IS. and Claesson, S. (1986) Isotopic evidence for the Precambrian provenance and Caledonian metamorphism of high grade paragneisses from the Seve Nappes, Scandinavian Caledonides. II: Ion microprobe zircon U-Th-Pb. Contributions to Mineralogy and Petrology, 97, 205–217.CrossRefGoogle Scholar
Winslow, D.M., Zeitler, P.K., Chamberlain, C.P. and Williams, I.S. (1996) Geochronological constraints on syntaxial development in the Nanga Parbat region, Pakistan. Tectonics, 15, 1292–1308.CrossRefGoogle Scholar
Zeck, H.P., Monie, P., Villa, I.M. and Hansen, B.T. (1992) Very high rates of cooling and uplift in the alpine belt of the Betic Cordillera, southern Spain. Geology, 20, 79–82.2.3.CO;2>CrossRefGoogle Scholar