Enrique, P. (Pere)2012-12-042012-12-0419900567-7505https://hdl.handle.net/2445/32989The 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 crust26 p.application/pdfeng(c) Enrique, P. (Pere), 1990Roques ígniesSerralada Litoral CatalanaIgneous rocksCatalan Coastal Range (Catalonia)info:eu-repo/semantics/article1971322012-12-04info:eu-repo/semantics/openAccess