Abstract
Abstract The Borne fault traversing the Borne granitic complex in the Central Massif, France, is characterized by evidence of renewed movement and successive phases of mineralization. Subsequent to injection of granulites, with which formation of the fault was associated, gold-and sulfide-bearing veins were formed. During the second phase of mineralization barite and some argentiferous galena were deposited in fractures of the fault zone. The final phase of mineralization was essentially one of fluorite formation.
Sign-in/Register to access full text options 
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.
