Formation of Olivine Veins by Reactive Fluid Flow in a Dehydrating Serpentinite

Abstract Many exposed high‐pressure meta‐serpentinites comprise a channelized network of olivine‐rich veins that formed during dehydration at depth and allowed the fluid to escape from the dehydrating rock. While previous studies have shown that chemical heterogeneities in rocks can control the form...

Full description

Bibliographic Details
Main Authors: K. Huber, J. C. Vrijmoed, T. John
Format: Article
Language:English
Published: Wiley 2022-06-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
Online Access:https://doi.org/10.1029/2021GC010267