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, Martin
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. Roč. 51, 1/2 (2010), s. 101-123. ISSN 0022-3530. E-ISSN 1460-2415
Impact factor: 3.842, year: 2010
http://hdl.handle.net/11104/0181823
Number of the records: 1