Abstract
Epimetamorphic ores which were collected on the dumps of the mining area Arzberg-Haufenreith show relicts and structures which point to a genesis of the type Meggen respectively Rammelsberg. Other arguments for this are mica-layers rich in Ilmenite, which are very probably representing basic metamorphic tuffs.
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 callSimilar Papers
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.
