Abstract
Abstract The uranium mineralization of the Saint-Pierre region consists of francevillite- impregnated fluviatile Oligocene sands deposited in a basin forming part of the regional Permo-Carboniferous coal-bearing trough developed in the crystalline basement complex of the Central Massif, France. The mineralization is considered syngenetic, and was probably controlled both by climatic and topographic conditions.
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.
