Present day serpentinization in New Caledonia, Oman and Yugoslavia
Geochimica et Cosmochimica Acta
By: I. Barnes, J. R. O’Neil, and J.J. Trescases
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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.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Present day serpentinization in New Caledonia, Oman and Yugoslavia |
| Series title | Geochimica et Cosmochimica Acta |
| DOI | 10.1016/0016-7037(78)90225-9 |
| Volume | 42 |
| Issue | 1 |
| Year Published | 1978 |
| Language | English |
| Publisher | Elsevier |
| Description | 2 p. |
| First page | 144 |
| Last page | 145 |