Titlebook: Hydrothermal Processes at Seafloor Spreading Centers; Peter A. Rona,Kurt Bostr?m,Kenneth L. Smith Book 1983 Springer Science+Business Medi

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Nato Conference Serieshttp://image.papertrans.cn/h/image/430521.jpg

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https://doi.org/10.1007/978-1-4899-0402-7bridge; convection; cooling; deposits; mass; metals; reading; research

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Preliminary Report on the Chemistry of Hydrothermal Solutions at 21° North, East Pacific Risemilar to basalts. The large resulting flux of non-radiogenic strontium is necessary to the overall isotopic balance of the element in the oceans. The close compositional agreement between the 21°N and Galapagos solutions provides further evidence for the validity of the general calculations developed using the Galapagos data.

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Reduced Gases and Bacteria in Hydrothermal Fluids: The Galapagos Spreading Center and 21°N East Pacid include organisms known to produce and consume the gases discussed here. We conclude that microbial activity in the warm GSC vents is a significant contributing factor in determining the final gas concentrations in the vent waters.

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Uptake and Transport of Heavy Metals by Heated Seawater: A Summary of the Experimental Results metals. Experiments with natural and evolved seawater (Mg and SO. depleted) at ≥400 C and 500 bars or 375°C and ~375 bars under rock-dominated conditions more closely reproduce the vent-water chemistry.

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