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This document summarizes research on mantle xenoliths from three localities in northeast Bavaria, Germany. Detailed analysis found the xenoliths experienced variable degrees (6-30%) of partial melting in the spinel stability field. They subsequently underwent metasomatism by alkaline and carbonate-rich melts, resulting in modal and cryptic metasomatism. Isotopic signatures suggest the metasomatizing melts incorporated some recycled crustal material like eclogite. Overall, the study provides insights into me

Author

clarklipman

Language

EN