Author(s)

Alexander Vasilyevich Tatarinov, Lyubov Ilyinichna Yalovik

Geological Institute Siberian Branch, Russian Academy of Sciences, Ulan-Ude, Russia.

It is shown that the ore-forming systems (OFS) of the Vendian-Riphean Greenstone belts (GSB) in the Transbaikalia region were formed in a wide age range: from the Riphean to the Cenozoic. They are grouped into 6 metallogenic types. The noble metal type is divided into 6 metallogenic subtypes differed in time duration intervals of functioning. OFS evolution wore multistage nature inherited from the composition of the GSB primary rocks, with a tendency of the ore generating processes remobilization and regeneration (dynamometamorphism) changing over time by rejuvenation (shoshonite latite and picrobasalt magmatism, mud volcanism).

Ore-Forming Systems, Noble Metals, Ore-Generating Processes, Dynamometamorphism, Age, Evolution

Tatarinov, A. and Yalovik, L. (2020) Ore Forming Systems (Fe, Ti, Ni, Pb, Zn, Noble Metals) of the Transbaikalia Neoproterozoic Greenstone Belts. Geomaterials, 10, 66-90. doi: 10.4236/gm.2020.103005.