Mantle-derived cargo or phenocrystic phases? Linking the texture and composition of olivine and phlogopite to the liquid line of descent of the Udachnaya kimberlite and the sub-cratonic mantle structure
- Casetta, F. (Speaker)
- Asenbaum, R. (Contributor)
- Igor Ashchepkov (Contributor)
- Olga Ageeva (Contributor)
- Theodoros Ntaflos (Contributor)
- Abart, R. (Contributor)
Activity: Talks and presentations › Poster presentation › Science to Science