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Present day serpentinization in New Caledonia,Oman and Yugoslavia
Authors:Ivan Barnes  JR O&#x;Neil  JJ Trescases
Institution:U.S. Geological Survey, Menlo Park, CA 94025, U.S.A.;Office de la Recherche Scientifique et Technique Outre-Mer, Paris, France
Abstract:Geochemical evidence for modern low-temperature serpentinization has been found in three new localities. Apparently the low-temperature reactions are a common mode of formation of the lizardite-chrysotile and brucite assemblage. Possibly the 18O content of serpentine formed at low temperatures is in part inherited from the pyroxene and olivine.
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