Fault geometry and permeability contrast control vent temperatures at the Logatchev 1 hydrothermal field, Mid-Atlantic Ridge

Author:

Andersen Christine,Rüpke Lars,Hasenclever Jörg,Grevemeyer Ingo,Petersen Sven

Publisher

Geological Society of America

Subject

Geology

Reference18 articles.

1. A method for quantitatively estimating diffuse and discrete hydrothermal discharge;Baker;Earth and Planetary Science Letters,1993

2. What processes at mid-ocean ridges tell us about volcanogenic massive sulfide deposits;Cathles;Mineralium Deposita,2011

3. Kinematics and geometry of active detachment faulting beneath the Trans-Atlantic Geotraverse (TAG) hydrothermal field on the Mid-Atlantic Ridge;deMartin;Geology,2007

4. The interplay of permeability and fluid properties as a first order control of heat transport, venting temperatures and venting salinities at mid-ocean ridge hydrothermal systems;Driesner;Geofluids,2010

5. Where are the large hydrothermal sulphide deposits in the oceans?: Philosophical Transactions of the Royal Society of London, Series A;Fouquet;Mathematical, Physical and Engineering Sciences,1997

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