摘要
For minerals containing multivalent elements,their stabilities depend not only on pressure(P),temperature(T),and bulk chemical composition,but also the redox state.This applies to many ore forming minerals,such that the redox state and its fluctuations in hydrothermal systems have long been considered as important controlling factors for the transport and deposition of ores.
For minerals containing multivalent elements,their stabilities depend not only on pressure(P),temperature(T),and bulk chemical composition,but also the redox state.This applies to many ore forming minerals,such that the redox state and its fluctuations in hydrothermal systems have long been considered as important controlling factors for the transport and deposition of ores.
出处
《矿物学报》
CAS
CSCD
北大核心
2013年第S2期561-561,共1页
Acta Mineralogica Sinica
基金
中国科学院知识创新工程领域前沿项目(批准号:SIDSSE-201302)
