作者: Pierre Barbey , Alain Cheilletz , Bernard Laumonier
DOI: 10.1016/S1251-8050(00)01506-8
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摘要: From new field and single zircon geochronological data, we reinterpret the structure of Canigou orthogneisses (Eastern Pyrenees) as an Early Ordovician rapakivi granite laccolith. This laccolith is surrounded by a contact metamorphic aureole predating Hercynian tectono-metamorphic events. consists migmatites at with unmelted orthogneisses, skarns in carbonate beds retrogressed Al-rich porphyroblasts over some hundred metres beyond contact. The metallogenic activity (Fe, F) observed around massif might be related to emplacement.