Present day serpentinization in New Caledonia, Oman and Yugoslavia
January 1, 1978
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.
Citation Information
| Publication Year | 1978 |
|---|---|
| Title | Present day serpentinization in New Caledonia, Oman and Yugoslavia |
| DOI | 10.1016/0016-7037(78)90225-9 |
| Authors | I. Barnes, J. O’Neil, J.J. Trescases |
| Publication Type | Article |
| Publication Subtype | Journal Article |
| Series Title | Geochimica et Cosmochimica Acta |
| Index ID | 70012766 |
| Record Source | USGS Publications Warehouse |