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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Bibliographic Details
Published inGeochimica et cosmochimica acta Vol. 292; pp. 285 - 308
Main Authors Lamadrid, H.M., Zajacz, Z., Klein, F., Bodnar, R.J.
Format Journal Article
LanguageEnglish
Published Elsevier Ltd 01.01.2021
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