Year-end Sale % OFF 
Abstract
The problematic crystalline complexes of the Saxon intermediate massif and of the gneiss massif of Münchberg in NE Bavaria, which appear abruptly in the Paleozoic series of a large synclinorium of the Saxothuringian zone in the German Variscan mountains, can be interpreted in the light of modern data and methods as pre-Variscan intruded laccolithic complexes which were altered into gneiss and sheared out divergently as autochthonous klippes in Variscan time.
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.
