Number of the records: 1
Two Contrasting Fabric Patterns of Olivine Observed in Garnet and Spinel Peridotite from a Mantle-derived Ultramafic Mass Enclosed in Felsic Granulite, the Moldanubian Zone, Czech Republic
- 1.Kamei, A., Obata, M., Michibayashi, K., Hirajima, T., Svojtka, M. Two Contrasting Fabric Patterns of Olivine Observed in Garnet and Spinel Peridotite from a Mantle-derived Ultramafic Mass Enclosed in Felsic Granulite, the Moldanubian Zone, Czech Republic. Journal of Petrology. 2010, 51(1/2), 101-123. ISSN 0022-3530. E-ISSN 1460-2415. Available: doi: 10.1093/petrology/egp092
Number of the records: 1