A capless 350 degrees C flow zone model to explain...

Economic Geology 1993 / 12 Vol. 88; Iss. 8

A capless 350 degrees C flow zone model to explain megaplumes, salinity variations, and high-temperature veins in ridge axis hydrothermal systems

Cathles, L. M.
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Volume:
88
Language:
english
Journal:
Economic Geology
DOI:
10.2113/gsecongeo.88.8.1977
Date:
December, 1993
File:
PDF, 346 KB
english, 1993
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