Ophiolite-Related Ultramafic Rocks (Serpentinites) in the Caribbean Region: A Review of their Occurrence, Composition, Origin, Emplacement and NiLaterite Soil Formation
Ultramafic rocks, mainly serpentinized peridotites of mantle origin, are mostly associated with the ophiolites ofMesozoic age that occur in belts along three of the margins of the Caribbean plate. The most extensive exposuresare in Cuba. The ultramafic-mafic association (ophiolites) were formed and...
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| Yayımlandı: | Geologica Acta: an international earth science journal |
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| Asıl Yazarlar: | , , , , |
| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
Universitat de Barcelona
2006
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| Konular: | |
| Online Erişim: | https://www.redalyc.org/articulo.oa?id=50540214 |
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