Abstract
In this paper the writer presents some considerations of the genesis of some cordierites in the cordierite bearing biotite migmatite and in the biotite bearing spinel cordierite oligoclasite and in the garnet bearing cordierite hypersthene biotite gneiss as well. The cordierite occurs as a product between the sheared porphyroclast of the plagioclase and the younger biotite which concentrates at the mechanical movement in the later stage of formation of every metamorphic rock.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
More From: The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists
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.