Effect of water activity on rates of serpentinization of olivine
Abstract
The hydrothermal alteration of mantle rocks (referred to as serpentinization) occurs in submarine environments extending from mid-ocean ridges to subduction zones. Serpentinization affects the physical and chemical properties of oceanic lithosphere, represents one of the major mechanisms driving mass exchange between the mantle and the Earth's surface, and is central to current origin of life hypotheses as well as the search for microbial life...
Paper Details
Title
Effect of water activity on rates of serpentinization of olivine
Published Date
Jul 14, 2017
Journal
Volume
8
Issue
1
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