Direct observation of a fossil high-temperature, fault-hosted, hydrothermal upflow zone in crust formed at the East Pacific Rise
Author:
Publisher
Geological Society of America
Subject
Geology
Link
http://pubs.geoscienceworld.org/geology/article-pdf/38/4/379/3539370/379.pdf
Reference35 articles.
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3. Strontium isotope constraints on fluid flow in the sheeted dike complex of fast spreading crust: Pervasive fluid flow at Pito Deep;Barker;Geochemistry Geophysics Geosystems,2008
4. An empirical equation of state for hydrothermal seawater (3.2 percent NaCl);Bischoff;American Journal of Science,1985
5. A simple magma-driven thermal balance model for the formation of volcanogenic massive sulphides;Cann;Earth and Planetary Science Letters,1985
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