Synthetic fluid inclusions XXIII. Effect of temperature and fluid composition on rates of serpentinization of olivine
Serpentinization, i.e. the hydrothermal alteration of ultramafic rocks, is an important and ubiquitous geologic process that occurs at slow- and ultraslow-spreading mid-ocean ridges, magma-poor passive margins, and subduction zones. While serpentinization occurs over a wide temperature range and inv...
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Published in | Geochimica et cosmochimica acta Vol. 292; pp. 285 - 308 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier Ltd
01.01.2021
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Subjects | |
Online Access | Get full text |
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