Drupal-Bibcite0<style face="normal" font="default" size="100%">P–T–t–d evolution of orogenic middle crust of the Roc de Frausa Massif (Eastern Pyrenees): A result of horizontal crustal flow and Carboniferous doming?</style><style face="normal" font="default" size="100%">P–T–t–d evolution of orogenic middle crust of the Roc de Frausa Massif (Eastern Pyrenees): A result of horizontal crustal flow and Carboniferous doming?</style>