Abstract
The Hospitalet mantled gneiss antiform consists of monzo-granitic
orthogneisses, which are overlain by a predominantly pelitic, at least
2.5 km thick succession of Cambro-Ordovician metasediments.
During the Hercynian orogeny the rocks were polyphase deformed and plurifacially
metamorphosed. Three stages in its tectonic evolution can be
distinguished.
Pre-antiform episode
NE-SW trending (Dl) folds were formed and overprinted by
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