Petrogenesis of the chromitite body from the Cerro Colorado ophiolite, Paraguaná Peninsula, Venezuela
Ultramafic-mafic rocks of ophiolitic affinity crop out along the Venezuelan Caribbean region. They have been interpreted as remnants of the oceanic lithosphere of the Caribbean volcanic arc (135-70 Ma) as well as relicts of proto-Caribbean oceanic lithosphere (Upper Jurassic-Lower Cretaceous) relate...
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| Vydáno v: | Boletín de la Sociedad Geológica Mexicana |
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| Hlavní autoři: | , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Sociedad Geológica Mexicana, A.C.
2020
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| Témata: | |
| On-line přístup: | https://www.redalyc.org/articulo.oa?id=94370787002 |
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