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Present day serpentinization in New Caledonia, Oman and Yugoslavia

Geochimica et Cosmochimica Acta

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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
Number of Pages:
2