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机构地区:[1]Department of Geology, Peking University, Beijing 100871, PRC
出 处:《Chinese Science Bulletin》1989年第24期2050-2054,共5页
基 金:Project supported by the National Natural Science Foundation of China (grant No. 4870203)
摘 要:Chou and Eugster and Boctor et al. studied the solubilities of magnetite and hematite, respectively, in supercritical HCl—H<sub>2</sub>O fluids using the foe and f<sub>HCl</sub> buffer tech niques. Crerar et al. determined the solubility of pyrite+pyrrhotite+magnetite in acidic NaCl hydrothermal solutions. These researches give principal experimental evidence for a prevailing hypothesis that Fe is transported as chloro-complexes in hydrothermal fluids. It
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