Abstract
A number of lines of evidence support the view that the gneissic host rock of the iron deposits is a product of granitization and that the iron deposits were formed by release of iron from ferromagnesian silicates during regional metamorphism. (See Buddington, ibid., v. 61, p. 484-510).
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.
