Abstract:The formation mechanism of the large hydrothermal sulfide deposit is a complex geological process involving many controlling factors. Mixing between hydrothermal fluid and seawater plays a key role in this process. The results of the Ocean Drilling Program (ODP) indicate that mixing of the evolved seawater and hydrothermal fluid, which is wildly developed within the Trans-Atlantic GeoTraverse (TAG) hydrothermal deposit, governs the internal structure and chemical compositions of the deposit to great extent. Ta… Show more
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