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OBATA, M. (1982) Reply to W. Schubert's Comments on the 'The Ronda Peridotite: Garnet--, Spinel--, and Plagicclase--Lherzolite Facies and The P--T Trajectories of a High-Temperature Mantle Intrusion'. Journal of Petrology, 23 (2) 296-298 doi:10.1093/petrology/23.2.296

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Reference TypeJournal (article/letter/editorial)
TitleReply to W. Schubert's Comments on the 'The Ronda Peridotite: Garnet--, Spinel--, and Plagicclase--Lherzolite Facies and The P--T Trajectories of a High-Temperature Mantle Intrusion'
JournalJournal of Petrology
AuthorsOBATA, M.Author
Year1982 (May 1)Volume23
Issue2
PublisherOxford University Press (OUP)
DOIdoi:10.1093/petrology/23.2.296Search in ResearchGate
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Mindat Ref. ID179849Long-form Identifiermindat:1:5:179849:8
GUID0
Full ReferenceOBATA, M. (1982) Reply to W. Schubert's Comments on the 'The Ronda Peridotite: Garnet--, Spinel--, and Plagicclase--Lherzolite Facies and The P--T Trajectories of a High-Temperature Mantle Intrusion'. Journal of Petrology, 23 (2) 296-298 doi:10.1093/petrology/23.2.296
Plain TextOBATA, M. (1982) Reply to W. Schubert's Comments on the 'The Ronda Peridotite: Garnet--, Spinel--, and Plagicclase--Lherzolite Facies and The P--T Trajectories of a High-Temperature Mantle Intrusion'. Journal of Petrology, 23 (2) 296-298 doi:10.1093/petrology/23.2.296
In(1982, May) Journal of Petrology Vol. 23 (2) Oxford University Press (OUP)

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SCHUBERT, W. (1982) Comments on 'The Ronda Peridotite: Garnet-, Spinel-, and Plagioclase-Lherzolite Facies and the P-T Trajectories of a High-Temperature Mantle Intrusion' by M. Obata (J. Petrology, 21, 533-72, 1980) Journal of Petrology, 23 (2) 293-295 doi:10.1093/petrology/23.2.293
MASAAKI, O. (1980) The Ronda Peridotite: Garnet-, Spinel-, and Plagioclase-Lherzolite Facies and the P-T Trajectories of a High-Temprature Mantle Intrusion. Journal of Petrology, 21 (3) 533-572 doi:10.1093/petrology/21.3.533
OBATA, M., MORTEN, L. (1987) Transformation of Spinel Lherzolite to Garnet Lherzolite in Ultramafic Lenses of the Austridic Crystalline Complex, Northern Italy. Journal of Petrology, 28 (3) 599-623 doi:10.1093/petrology/28.3.599
LORAND, J P. (1989) Sulfide Petrology of Spinel and Garnet Pyroxenite Layers from Mantle-derived Spinel Lherzolite Massifs of Arieg`, Northeastern Pyrenees, France. Journal of Petrology, 30 (4) 987-1015 doi:10.1093/petrology/30.4.987
Kamei, A., Obata, M., Michibayashi, K., Hirajima, T., Svojtka, M. (2010) 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, 51 (1) 101-123 doi:10.1093/petrology/egp092
IONOV, D. (2004) Chemical Variations in Peridotite Xenoliths from Vitim, Siberia: Inferences for REE and Hf Behaviour in the Garnet-Facies Upper Mantle. Journal of Petrology, 45 (2) 343-367 doi:10.1093/petrology/egg090
OBATA, M. (1994) Material Transfer and Local Equilibria in a Zoned Kelyphite from a Garnet Pyroxenite, Ronda, Spain. Journal of Petrology, 35 (1) 271-287 doi:10.1093/petrology/35.1.271
EHRENBERG, S. N. (1982) Petrogenesis of Garnet Lherzolite and Megacrystalline Nodules from the Thumb, Navajo Volcanic Field. Journal of Petrology, 23 (4) 507-547 doi:10.1093/petrology/23.4.507
IONOV, D. A., ASHCHEPKOV, I. V., STOSCH, H.-G., WITT-EICKSCHEN, G., SECK, H. A. (1993) Garnet Peridotite Xenoliths from the Vitim Volcanic Field, Baikal Region: the Nature of the Garnet--Spinel Peridotite Transition Zone in the Continental Mantle. Journal of Petrology, 34 (6) 1141-1175 doi:10.1093/petrology/34.6.1141
Kaekane, Jarious B, Proyer, Alexander (2022) Clues from Garnet-Spinel-Bearing Peridotite and Pyroxenite Xenoliths about the Formation of the Subcratonic Lithospheric Mantle—a Case Study from the Orapa Kimberlite Cluster. Journal of Petrology, 63 (7) doi:10.1093/petrology/egac058
OBATA, M. (2004) Compositional Continuity and Discontinuity in the Horoman Peridotite, Japan, and its Implication for Melt Extraction Processes in Partially Molten Upper Mantle. Journal of Petrology, 45 (2) 223-234 doi:10.1093/petrology/egg106
 
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