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Omori, S., Kita, S., Maruyama, S., Santosh, M. (2009) Pressure–temperature conditions of ongoing regional metamorphism beneath the Japanese Islands. Gondwana Research, 16 (3) 458-469 doi:10.1016/j.gr.2009.07.003

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Reference TypeJournal (article/letter/editorial)
TitlePressure–temperature conditions of ongoing regional metamorphism beneath the Japanese Islands
JournalGondwana Research
AuthorsOmori, S.Author
Kita, S.Author
Maruyama, S.Author
Santosh, M.Author
Year2009 (December)Volume16
Issue3
PublisherElsevier BV
URL
DOIdoi:10.1016/j.gr.2009.07.003Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID711593Long-form Identifiermindat:1:5:711593:0
GUID0
Full ReferenceOmori, S., Kita, S., Maruyama, S., Santosh, M. (2009) Pressure–temperature conditions of ongoing regional metamorphism beneath the Japanese Islands. Gondwana Research, 16 (3) 458-469 doi:10.1016/j.gr.2009.07.003
Plain TextOmori, S., Kita, S., Maruyama, S., Santosh, M. (2009) Pressure–temperature conditions of ongoing regional metamorphism beneath the Japanese Islands. Gondwana Research, 16 (3) 458-469 doi:10.1016/j.gr.2009.07.003
In(2009, December) Gondwana Research Vol. 16 (3) Elsevier BV

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Zhao, Dapeng, Santosh, M., Maruyama, Shigenori (2009) Tectonics of the Japanese Islands and surrounding regions: Introduction. Gondwana Research, 16 (3) 365-367 doi:10.1016/j.gr.2009.07.004
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Maruyama, S., Santosh, M. (2007) Island arcs: Past and present. Gondwana Research, 11 (1) 3-6 doi:10.1016/j.gr.2006.10.001
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Maruyama, S., Santosh, M. (2010) A tribute to Akiho Miyashiro: Introduction. Gondwana Research, 18 (1) 1-3 doi:10.1016/j.gr.2010.03.008
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MARUYAMA, Shigenori, OMORI, Soichi, IWASE, Yasuyuki (2004) On-going Regional Metamorphism beneath the Japanese Islands. Journal of Geography (Chigaku Zasshi), 113 (5) 600-616 doi:10.5026/jgeography.113.5_600
Maruyama, Shigenori, Masago, H., Katayama, I., Iwase, Y., Toriumi, M., Omori, S., Aoki, K., (2010) A new perspective on metamorphism and metamorphic belts☆. Gondwana Research, 18 (1) 106-137 doi:10.1016/j.gr.2010.03.007
 
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