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The Hercynian intrusive rocks of the Catalonian Coastal Ranges (NE Spain).
Enrique, P. (Pere)
Universitat de Barcelona
The hercynian outcrops of the Catalonian Coastal Ranges (NE Spain) consist mainly of Lower Permian-Upper Carboniferous, post-tectonic, epizona1 granitoid intrusions which form a typical applutonic calc-alkaline suite ranging from mafic hornblende gabbros and ultramafic olivine homblendites throught on alites and granodioritcs to leucogranites. This suite displays major andtrace-element characteristics and Sr isotope ratios similar to volcanic arc and post-collision magmatism oceanic lithosphere and to have been modified by contamination and is therefore believed to have formed above subducted with melts from the crust
-Roques ígnies
-Serralada Litoral Catalana
-Igneous rocks
-Catalan Coastal Range (Catalonia)
(c) Enrique, P. (Pere), 1990
Article
Article - Versió publicada
Universitat de Barcelona (UB). Institut de Cièncias de la Terra Jaume Almera (ICTJA)
         

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