Abstract
Abstract Several horizons, well defined on the basis of their micrographic and micropaleontologic characteristics, are recognized in the Senonian (Cretaceous) sediments traversed by excavations for the gas line northward from the Lacq field in Charente toward the center of France. Precise stratigraphic definition of the zones was possible with the aid of associated ammonites and species of Inoceramus.
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 callSimilar Papers
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.
