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Diagenesis in the volcaniclastic sequences of Western Nicaragua: Mineralogical Breaks and Tectónic implications.

1995

G5-0034

Southwestern Nicaragua is made up of several Cretaceous to Cenozoic stratigraphic units consisting of sedimentary rocks resting on a aphiolitic basement of Jurassict to mid-Cretaceous age. The sedimentary sequence is dominated by colcaniclastic rocks which represent a Shallowing-up succesion from deep marine turbidities to Shallow marine and continental deposits.

Ministerio de Energía y Minas - Centro de Documentación

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