Abstract
Along the Northern Calcareous Alps (NCA) and Southern Alps (SA) more than 1000 m thick carbonate ramps, platforms and basinal deposits developed in transtensional rifted basins. New ammonite and conodont data and the sequence-stratigraphic reinterpretation of already well known sections allow a first comparison of sequence boundaries and flooding surfaces in NCA and SA.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: 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.