Hydrothermal fluid fluxes calculated from the isotopic mass balance of thallium in the ocean crust
Hydrothermal fluids expelled from the seafloor at high and low temperatures play pivotal roles in controlling seawater chemistry. However, the magnitude of the high temperature water flux of mid-ocean ridge axes remains widely disputed and the volume of low temperature vent fluids at ridge flanks is...
| Main Authors: | , , , , , |
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| 格式: | Journal article |
| 语言: | English |
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Elsevier
2006
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