Rodgers, K. A. (1974) Serpentine minerals from the southern portion of the ultramafic belt of New Caledonia. Mineralogical Magazine, 39 (307) 798-801 doi:10.1180/minmag.1974.039.307.07
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Serpentine minerals from the southern portion of the ultramafic belt of New Caledonia | ||
| Journal | Mineralogical Magazine | ||
| Authors | Rodgers, K. A. | Author | |
| Year | 1974 (September) | Volume | 39 |
| Issue | 307 | ||
| Publisher | Mineralogical Society | ||
| Download URL | https://rruff.info/doclib/MinMag/Volume_39/39-307-798.pdf+ | ||
| DOI | doi:10.1180/minmag.1974.039.307.07Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 6782 | Long-form Identifier | mindat:1:5:6782:3 |
| GUID | 0 | ||
| Full Reference | Rodgers, K. A. (1974) Serpentine minerals from the southern portion of the ultramafic belt of New Caledonia. Mineralogical Magazine, 39 (307) 798-801 doi:10.1180/minmag.1974.039.307.07 | ||
| Plain Text | Rodgers, K. A. (1974) Serpentine minerals from the southern portion of the ultramafic belt of New Caledonia. Mineralogical Magazine, 39 (307) 798-801 doi:10.1180/minmag.1974.039.307.07 | ||
| In | (1974, September) Mineralogical Magazine Vol. 39 (307) Mineralogical Society | ||
| Abstract/Notes | SummaryPeridotitic rocks in the Massif du Sud, southern New Caledonia, have suffered about 30 % serpentinization. Optical studies combined with X-ray and chemical analyses indicate that chrysotile and lizardite are the dominant serpentine species present. Serpentinization probably occurred during emplacement of the Massifs in their present overthrust position. | ||
See Also
These are possibly similar items as determined by title/reference text matching only.
 | |
 | |
 | |
 | |
 | |
 | |
| |
 | |
 | |
 | |
 |