Redox Control and Measurements in Hydrothermal Experiments  

作　　者：CHOU I-Ming 

机构地区：[1]Laboratory for Experimental Study Under Deep-sea Extreme Conditions, Sanya Institute of Deep-sea Science and Engineering,Chinese Academy of Sciences

出　　处：《矿物学报》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)

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.

关 键 词：redox MINERALS HYDROTHERMAL KINETICS sealed PERMEATION DISSOCIATION mentioned CAPSULE adding 

分 类 号：X703[环境科学与工程—环境工程]