Abstract
The block-faulted southwestern margin of the Bohemian Massif is superimposed on a Permo-Carboniferous graben, major faults of which became repeatedly reactivated during the Mesozoic and Cenozoic. Inversion of sedimentary basins associated with this fault system occurred during the Early Cretaceous and again during the latest Cretaceous-Early Cenozoic.
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.
