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Yokoyama, Kazumi (1980) Nikubuchi peridotite body in the sanbagawa metamorphic belt; thermal history of the ?Al-pyroxene-rich suite? peridotite body in high pressure metamorphic terrain. Contributions to Mineralogy and Petrology, 73 (1) 1-13 doi:10.1007/bf00376256

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Reference TypeJournal (article/letter/editorial)
TitleNikubuchi peridotite body in the sanbagawa metamorphic belt; thermal history of the ?Al-pyroxene-rich suite? peridotite body in high pressure metamorphic terrain
JournalContributions to Mineralogy and Petrology
AuthorsYokoyama, KazumiAuthor
Year1980 (June)Volume73
Issue1
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/bf00376256Search in ResearchGate
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Mindat Ref. ID74962Long-form Identifiermindat:1:5:74962:6
GUID0
Full ReferenceYokoyama, Kazumi (1980) Nikubuchi peridotite body in the sanbagawa metamorphic belt; thermal history of the ?Al-pyroxene-rich suite? peridotite body in high pressure metamorphic terrain. Contributions to Mineralogy and Petrology, 73 (1) 1-13 doi:10.1007/bf00376256
Plain TextYokoyama, Kazumi (1980) Nikubuchi peridotite body in the sanbagawa metamorphic belt; thermal history of the ?Al-pyroxene-rich suite? peridotite body in high pressure metamorphic terrain. Contributions to Mineralogy and Petrology, 73 (1) 1-13 doi:10.1007/bf00376256
In(1980, June) Contributions to Mineralogy and Petrology Vol. 73 (1) Springer Science and Business Media LLC

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Itaya, Tetsumaru, Banno, Shohei (1980) Paragenesis of titanium-bearing accessories in pelitic schists of the Sanbagawa metamorphic belt, Central Shikoku, Japan. Contributions to Mineralogy and Petrology, 73 (3) 267-276 doi:10.1007/bf00381445
Sakakibara, M., Isono, Y. (1996) Middle Miocene thermal metamorphism due to the infiltration of high-temperature fluid in the Sanbagawa metamorphic belt, southwest Japan. Contributions to Mineralogy and Petrology, 125 (4) 341-358 doi:10.1007/s004100050227
ENAMI, M. (1983) Petrology of pelitic schists in the oligoclase-biotite zone of the Sanbagawa metamorphic terrain, Japan: phase equilibria in the highest grade zone of a high-pressure intermediate type of metamorphic belt. Journal of Metamorphic Geology, 1 (2) 141-161 doi:10.1111/j.1525-1314.1983.tb00269.x
YANG, J. S, ZHANG, R. Y., LI, T. F., ZHANG, Zh. M., LIOU, J. G. (2007) Petrogenesis of the garnet peridotite and garnet-free peridotite of the Zhimafang ultramafic body in the Sulu ultrahigh-pressure metamorphic belt, eastern China. Journal of Metamorphic Geology, 25 (2) 187-206 doi:10.1111/j.1525-1314.2006.00688.x
Ota, T (2004) Thermobaric structure and metamorphic evolution of the Iratsu eclogite body in the Sanbagawa belt, central Shikoku, Japan. Lithos, 73 (1) 95-126 doi:10.1016/j.lithos.2004.01.001
YOSHIDA, D. (2004) Pressure-Temperature Path Recorded in the Yangkou Garnet Peridotite, in Su-Lu Ultrahigh-pressure Metamorphic Belt, Eastern China. Journal of Petrology, 45 (6) 1125-1145 doi:10.1093/petrology/egh008
KUNUGIZA, KEITARO (1981) Two contrasting types of zoned chromite of the Mt. Higashi-Akaishi peridotite body of the Sanbagawa metamorphic belt, central Shikoku. The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists, 76 (10) 331-342 doi:10.2465/ganko1941.76.331
Enami, Masaki, Wallis, Simon R., Banno, Yasuyuki (1994) Paragenesis of sodic pyroxene-bearing quartz schists: implications for the P-T history of the Sanbagawa belt. Contributions to Mineralogy and Petrology, 116 (1) 182-198 doi:10.1007/bf00310699
Enami, Masaki, Wakasugi, Yuki, Tsuboi, Motohiro (2021) Local CO2 variation and evolution of metamorphic fluid at the lithologic boundary recorded in Sanbagawa metamorphic rocks, Central Shikoku, Japan. Contributions to Mineralogy and Petrology, 176 (8) doi:10.1007/s00410-021-01817-1
Jaques, A. L., Green, D. H. (1980) Anhydrous melting of peridotite at 0?15 Kb pressure and the genesis of tholeiitic basalts. Contributions to Mineralogy and Petrology, 73 (3) 287-310 doi:10.1007/bf00381447
Frick, C. (1973) The sulphides in griquaite and garnet-peridotite xenoliths in kimberlite. Contributions to Mineralogy and Petrology, 39 (1) 1-16 doi:10.1007/bf00374242
 
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