Abstract
A Possible Evolutionary Model of Apuseni Mountains and of Biharia Nappe System. Our intention is to expose and outline a possible structural model for the Paleozoic evolution of the Apuseni Mountains and for the alpine evolution of some tectonic units belonging to the Biharia Nappe System. During the Paleozoic times, the tectonic units involved in this model migrated from the northern margin of Gondwana toward Laurasia, then collided in Variscan orogeny. The Biharia and Codru Nappe Systems were sheared from the Preapulian craton margins, and the Transylvanides were sheared from the Penninic rift, during the Alpine orogeny.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
