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Present day serpentinization in New Caledonia, Oman and Yugoslavia

Geochimica et Cosmochimica Acta
By: , and 

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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. ?? 1978.

Additional publication details

Publication type Article
Publication Subtype Journal Article
Title Present day serpentinization in New Caledonia, Oman and Yugoslavia
Series title Geochimica et Cosmochimica Acta
Volume 42
Issue 1
Year Published 1978
Language English
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Geochimica et Cosmochimica Acta
First page 144
Last page 145