Caribbean Plate margin evolution: constraints and current problems
Oceanic crust was generated at multiple spreading centres during the Jurassic and Early Cretaceous, forming aproto-Caribbean oceanic domain. During the Cretaceous, part of that crustal domain thickened into an oceanicplateau, of petrologic Mid-Ocean Ridge (MOR) to Ocean Island Basalt (OIB) affinit...
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| Publicado no: | Geologica Acta: an international earth science journal |
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| Principais autores: | , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Universitat de Barcelona
2006
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| Acesso em linha: | https://www.redalyc.org/articulo.oa?id=50540215 |
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