Abstract
Mineral deposits exhibit extremely heterogeneous distributions, with each major deposit type showing a distinctive, commonly unique, temporal pattern. Individual temporal patterns reflect a complex interplay between formational and preservational forces that, in turn, largely reflect changes in tectonic processes and environmental conditions in an evolving Earth. The first-order drivers were the super continent cycle and evolution from plume-dominated to modern-style plate tectonics in a cooling Earth. Consequent decrease in the growth rate of continental crust, and change from thick, buoyant sub-continental lithospheric mantle (SCLM) in the Precambrian to thinner, negatively buoyant SCLM in the Phanerozoic, led to progressive decoupling of formational and preservational processes through time. This affected the temporal patterns of deposit types including orogenic gold, porphyry and epithermal deposits, VHMS, palaeoplacer Au, iron-oxide Cu-Au, PGE, diamond and probably SEDEX deposits.
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References
Abbott DH, Isley AE (2002) The intensity, occurrence and duration of superplume events and eras over geological time. Journal of Geodynamics 34: 265–307
Barley ME, Groves DI (1992) Supercontinent cycles and the distribution of metal deposits through time. Geology 20: 291–294
Betts PG, Giles D, Lister GS, Frick LR (2002) Evolution of the Australian lithosphere. Australian Journal of Earth Sciences 49: 661–695
Condie KC (2000) Episodic continental growth models: afterthoughts and extensions. Tectonophysics 322: 153–162
Condie KC (in press) Supercontinents and superplume events: distingushing signals in the geologic record? Physics of the Earth and Planets International
Frimmel HE, Groves DI, Kirk J, Ruiz J, Chesley J, Minter WEL (in press) The formation and preservation of the Witwatersrand goldfields, the largest gold province, in the world. Economic Geology
Goldfarb RJ, Groves EI, Gardoll S (2001) Orogenic gold and geologic time: A global synthesis. Ore Geology Review 18: 1–75
Griffin WL, O’Reilly SY, Abe N, Aulbach S, Davies RM, Pearson NJ, Doyle BJ, Kivi K (2003) The origin and evolution of Archean lithospheric mantle. Precambrian Research 127: 19–41
Groves DI, Ho SE, Rock NMS, Barley ME, Muggeridge MY (1987) Archean cratons, diamond and platinum; evidence for coppled long lived crust-mantle systems. Geology 15: 801–805
Groves DI, Vielreicher RM, Goldfarb RJ, Condie KC (in press a) Controls on the heterogeneous distribution of mineral deposits through time. Journal of the Geological Society
Groves DI, Condie KC, Goldfarb RJ, Hronsky JMA, Vielreicher RM (in press b) Secular changes in global tectonic processes and their influence on the temporal distribution of gold-bearing mineral deposits. Economic Geology
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© 2005 Springer-Verlag Berlin Heidelberg
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Groves, D.I., Vielreicher, R.M., Goldfarb, R.J., Hronsky, J.M.A., Condie, K.C. (2005). Tectonic and lithospheric controls on the heterogeneous temporal distribution of mineral deposits. In: Mao, J., Bierlein, F.P. (eds) Mineral Deposit Research: Meeting the Global Challenge. Springer, Berlin, Heidelberg. https://doi.org/10.1007/3-540-27946-6_3
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DOI: https://doi.org/10.1007/3-540-27946-6_3
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