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Date: 2013-09-17 04:43:55Igneous rocks Economic geology Structure of the Earth Anorthosite Archean Shear zone Diapir Tectonophysics Layered intrusion Geology Petrology Structural geology | ELSEVIER Tectonophysics[removed]–130 The deformation of the Egersund–Ogna anorthosite massif, south Norway: finite-element modelling of diapirismAdd to Reading ListSource URL: orbi.ulg.ac.beDownload Document from Source WebsiteFile Size: 4,39 MBShare Document on Facebook |