Abstract
On the magnetite and the hematite from the cupriferous iron sulphide deposits, such as the Shingü, Shirataki, Sazare, and Kõtsu mines, occurring in the Sambagawa crystalline schist zone, the writer has chiefly investigated occurrence, various textures under the ore-microscope distribution of minor elements and magnetic property. It is the purpose of this paper to give some interpretation on the genesis of Kieslager.
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 callMore 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.
