Abstract
The tectonic evolution of the Earth is the leading factor that accounts for the uneven distribution of lead and zinc reserves through geologic time. The cyclic changes in lead–zinc ore formation productivity reflected the periodic amalgamation of most continental crustal blocks and supercontinent formation, stabilization, and eventual breakup. Many features of the age spectra of lead and zinc reserves are caused by the gradual growth of the continental crust as a result of the accretion of island arcs to the cratonic nuclei, the widening extent of the ensialic environments of ore formation, and the increasing role of the continental crust in magma generation processes.
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REFERENCES
Barley, M.E. and Groves, D.I., Supercontinental cycles and the distribution of metal deposits through time, Geology, 1992, no. 20, pp. 291–302.
Bozhko, N.A., On two types of supercontinental cyclicity, Moscow Univ. Geol. Bull., 2011, vol. 66, no. 5, pp. 313–322.
Bradley, D.C., Passive margins through earth history, Earth-Sci. Rev., 2008, vol. 91, pp. 1–26.
Cawood, P.A., Kroner, A., and Pisarevsky, S., Precambrian plate tectonics: criteria and evidence, GSA Today, 2006, vol. 16, no. 7, pp. 4–11.
Condie, K.C., Episodic continental growth and supercontinents: a mantle avalanche connection? Earth Planet. Sci. Lett., 1998, vol. 163, pp. 97–108.
Davidson, A., Late Paleoproterozoic to mid-Neoproterozoic history of northern Laurentia: An overview of central Rodinia, Precambrian Res., 2008, vol. 160, pp. 5–22.
Dergachev, A.L., Eremin, N.I., and Sergeeva, N.E., Different-scale tendencies of the evolution of the composition of volcanogenic pyrite deposit ore, Moscow Univ. Geol. Bull., 2013, no. 5, pp. 31–40.
Dergachev, A.L., Dergachev, A.A., and Eremin, N.I., Epochs of zinc–lead ore formation in the geological history of the Earth, Moscow Univ. Geol. Bull., 2015, vol. 70, no. 3, pp. 240–249.
Eremin, N.I., Dergachev, A.L., Pozdnyakova, N.V., and Sergeeva, N.E., Epochs of volcanic-hosted massive sulfide ore formation in the Earth’s history, Geol. Ore Deposits, 2002, vol. 44, no. 4, pp. 259–275.
Evans, D.A.D., Reconstructing pre-Pangean supercontinents, Geol. Soc. Am. Bull., 2013, vol. 125, pp. 1735–1751.
Li, Z.X., Bogdanova, S.V., Collins, A.S., Davidson, A., et al., Assembly, configuration, and break-up history of Rodinia: a synthesis, Precambrian Res., 2008, vol. 160, pp. 179–210.
Meyer, C., Ore metals through geologic history, Science, 1985, vol. 227, pp. 1421–1428.
Meyer, C., Ore deposits as guides to geologic history of the Earth, Ann.Rev. Earth Sci., 1988, vol. 16, pp. 147–171.
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Translated by E. Murashova
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Dergachev, A.L. The Global Factors of Lead–Zinc Ore Formation. Moscow Univ. Geol. Bull. 74, 433–440 (2019). https://doi.org/10.3103/S0145875219050041
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DOI: https://doi.org/10.3103/S0145875219050041