Abstract
Abstract Pitchblende, hematite, and chlorite are formed in a large carbonate breccia consisting partly of greenstones and greenschists, partly of albite-rich rocks of several kinds. One of the latter, a coarse-grained albite »syenite» contains the uranium mineralization, while hematite is common in the whole breccia. The genesis of the pitchblende mineralization is discussed in relation to the main petrogenic processes of the orogeny: the granitization, the carbonatization, and the albite rock formation. The close spatial relationship of pitchblende and albite »syenite» indicates a close genetic relationship.
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.
