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J-GLOBAL ID:201702227341155795   Reference number:17A1738609

Serpentinization and blueschist-facies metamorphism beneath the Mariana forearc

マリアナ前弧域直下の蛇紋岩化作用と低温高圧型変成作用
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Volume: 123  Issue: 10  Page: 907-919  Publication year: Oct. 15, 2017 
JST Material Number: F0528A  ISSN: 0016-7630  CODEN: CHTZA5  Document type: Article
Article type: 原著論文  Country of issue: Japan (JPN)  Language: JAPANESE (JA)
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Petrogenesis 
Reference (56):
  • Aoya, M., Endo, S., Mizukami, T. and Wallis, S. R., 2013, Paleo-mantle wedge preserved in the Sambagawa high-pressure metamorphic belt and the thickness of forearc continental crust. Geology, 41, 451-454.
  • 坂野昇平・鳥海光弘・小畑正明(Banno, S., Toriumi, M., Obata, M., and Nishiyama, T.), 2000, 岩石形成のダイナミクス(Dynamics of Petrogenesis). 東京大学出版会(Univ. Tokyo Press), 320 p.
  • Brown, E. H. and Ghent, E. D., 1983, Mineralogy and phase relations in the blueschist facies of the Black Butte and Ball Rock areas, northern California Coast Ranges. Amer. Mineral., 68, 365-372.
  • Cloos, M. and Shreve, R. L., 1988a, Subduction-channel model of prism accretion, melange formation, sediment subduction, and subduction erosion at convergent plate margins: 1. Background and Description. Pure Appl. Geophys., 128, 455-500.
  • Cloos, M. and Shreve, R. L., 1988b, Subduction-channel model of prism accretion, melange formation, sediment subduction, and subduction erosion at convergent plate margins: 2. Implications and Discussion. Pure Appl. Geophys., 128, 501-545.
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