Diffuse flows of high-temperature fluids and their role in the formation of hydrothermal deposits

被引:0
|
作者
Yu. A. Bogdanov
A. Yu. Lein
O. Yu. Bogdanova
N. V. Ul’yanova
机构
[1] Russian Academy of Sciences,Shirshov Institute of Oceanology
来源
Oceanology | 2012年 / 52卷
关键词
Massive Sulfide; Diffuse Flow; Hydrothermal Field; Hydrothermal Deposit; Concentrate Flow;
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学科分类号
摘要
The compositions of the hydrothermal deposits formed at the oceanic bottom by diffuse and concentrated high-temperature hydrothermal flows are highly variable. The role of these flows in the formation of hydrothermal ores varies depending on the maturity of the hydrothermal mounds, the volcanism, and other factors. The average composition of the mature hydrothermal deposits is largely determined by the diffuse fluxes of hydrothermal fluids rather than by their concentrated flows.
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页码:655 / 665
页数:10
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