Genesis of early Precambrian complexes and of theirs metallogeny according to data of hot heterogeneous accretion of the Earth
https://doi.org/10.31242/2618-9712-2019-24-1-43-51
Abstract
It was shown that modern evidence of global magma ocean fractionation during Earth accretion allow to explain discussion problems of Early Precambrian. Due to a relatively low pressure during fractionation early magma ocean its mainly residual melts have acid composition. This provided acid composition mainly Early Precambrian rocks. Origin from melts explain high temperature crystallization these rocks. Dipping of cold rocks and sediments caused origin of heterogeneous complexes. Raising of deep migmas caused presence of high-baric rocks and very ancient age of basic crystalline schists. Emanation and magmatic differentiation of magma ocean caused origin of unique deposits.
About the Author
V. S. ShkodzinskiyRussian Federation
SHKODZINSKIY Vladimir Stepanovich, Doctor of Geological and Mineralogical Sciences, Leading Researcher, Diamond and Precious Metal Geology Institute SB RAS, 39, pr. Lenina, Yakutsk, 677980, Russia, https://orcid.org/0000-0001-7749-1264, shkodzinskiy@diamond.ysn.ru.
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Review
For citations:
Shkodzinskiy V.S. Genesis of early Precambrian complexes and of theirs metallogeny according to data of hot heterogeneous accretion of the Earth. Arctic and Subarctic Natural Resources. 2019;24(1):43-51. (In Russ.) https://doi.org/10.31242/2618-9712-2019-24-1-43-51