Answers are grounded in this paper and cite their sources.
Demonstrates the role of volatiles in ore mineralization, highlighting fluid sources in a geological context.
A role of volatiles at some stages of development of ore-magmatic system (OMS) in the Erdenetuin-Obo deposit is characterized by data of gas chromatography. The deep-seated source of the third stage fluids is considered most important. The fluid- and ore-generating role of an intermediate source is highlighted. It is connected with porphyry magmatism manifestation. Ore mineralization evolution was promoted by an increased oxidation potential at the second stage of OMS development.
No takes yet. Share an insight, caveat, or question.
Berzina et al. (1991) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: