Abstract
Major types of mineral deposits exhibit distinct changes in composition and geological setting from Archean to Recent time. These changes include extinctions of ancient types, appearances of new ones, proliferations, and diversifications, and thus are comparable to those seen in biological evolution. The changes are responses to evolutionary changes in the earth’s asthenosphere, lithosphere, hydrosphere, atmosphere and biosphere. All these reflect changing geotectonic environments, and consequently must be considered and explained in conjunction with global tectonic evolution, to which they provide additional, independent guides.
Explanations for the evolutionary changes in the type of deposits are conjectural due to the complexity and imperfect understanding of the processes that form many of them. However, changes in magmatic deposits of Cr, Ni — Cu, and Pt-Group elements may result from changes through time in subcrustal conditions and processes deep within the earth; e.g. changes in core/mantle compositi ns and boundaries, heat flux, or depth and degree of partial melting. Since about 1 Ga B.P., lithospheric evolution by plate tectonic processes, from initial oceanic crust across continent-margin environments to final, stabilized continental crust, has been paramount and has governed the nature of the hydrothermal systems that form many metalliferous deposits. It has thereby resulted in sequential evolutionary formation of many different types of deposits in these differing supracrustal settings.
An analogous, but temporally much longer and global evolution of lithosphere may be represented by sequential changes from Early to Late Archean greenstone belts, then through latest Archean plutonism and crustal stabilization to the diverse continental crustal tectonic environments of Proterozoic time. This longer term lithospheric evolution also controlled the development of differing types of deposits during the long span of Precambrian time. A remarkable absence of certain earlier types and the appearance and proliferation of certain new ones, or variants, in Mid-Proterozoic time suggests widespread, even global crustal rifting -perhaps due to global expansion.
Atmospheric-hydrospheric oxygenation, probably due to biogenic evolution in Lower Proterozoic time, profoundly altered the nature of ferruginous sedimentary rocks and their contained iron deposits. Primitive algal forms apparently played a role in formation of the great Au deposits of the Witwatersrand, and the appearance of terrestrial organisms in Mid-Paleozoic time created an environment favorable for generation of certain U deposits.
If ore deposits of different types have developed in response to evolutionary changes on the earth, it becomes imperative to explore for them not only in the proper spatial or geological environment but also in the proper time dimension, or age of rock. It would be disastrous to seek trilobites in Cretaceous marine shales or dinosaur bones in Silurian continental clastic sediments. Time, as expressed by geologic age, is of qual importance in mineral exploration.
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Hutchinson, R.W. (1992). Mineral Deposits and Metallogeny: Indicators of Earth’s Evolution. In: Schidlowski, M., Golubic, S., Kimberley, M.M., McKirdy, D.M., Trudinger, P.A. (eds) Early Organic Evolution. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-76884-2_42
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