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MEDIUM-PRESSURE METAMORPHISM IN THE CENTRAL SANTANDER MASSIF, EASTERN CORDILLERA, COLOMBIAN ANDES

The Central Santander Massif exposes its metamorphic basement, which mainly consists of medium- to high-grade pelitic schists, paragneisses, migmatites and orthogneisses. For delineating its metamorphic evolution, we have examinated mineral assemblages, metamorphic reactions and P-T conditions of me...

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Bibliografske podrobnosti
izdano v:Boletín de Geología
Principais autores: C. A. García, C. A. Ríos, O. M. Castellanos
Format: Artigo
Jezik:Inglês
Izdano: Universidad Industrial de Santander 2005
Teme:
Online dostop:https://www.redalyc.org/articulo.oa?id=349631990004
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