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Home Publications 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?

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?

Publication Type Journal Article
Author Carmen Aguilar, M Liesa, Pavla Štípská, Karel Schulmann, J.A Munoz, J.M Casas
Year of Publication 2015
Journal Journal of Metamorphic Geology
Volume 33
Number of Pages 273-294
Date Published 04/2015
DOI 10.1111/jmg.12120
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