Abstract
THERE is a growing body of evidence which supports the hypothesis of a counterclockwise rotation of Corsica and Sardinia with respect to southern France, in particular the palaeomagnetic data from the Permo-Carboniferous of Corsica1,2 and the Permian and Oligo-Miocene of Sardinia3–4. Although it has been suggested that the rotation possibly took place as early as the Mesozoic2, it is now more generally regarded as having occurred at some time during the Tertiary6,7.
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.