Abstract
A trilobite assemblage found in greenish gray argillites in the western El Baul massif, Venezuela, makes it possible to assign a Paleozoic age to the enclosing rocks, here defined as the Mireles formation. The argillites had previously been included in the group of rocks described as El Baul metamorphics, for which a Triassic-Jurassic age had been postulated.
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.
