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表紙
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まえがき
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目次
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The formation of the Hida nappe and the tectonics of Mesozoic sediments : The tectonic evolution of the Hida region, Central Japan
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1-20
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Geochemical investigation of the Hida metamorphic rocks
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21-37
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Structure and tectonics of the Hida massif, central Japan
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39-62
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Time-relationship between deformation and metamorphism of the Ogcheon zone in the Ogcheon district, South Korea
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63-90
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Tectono-metamorphic processes of the Ryoke belt in the Iwakuni-Yanai district, southwest Japan
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91-120
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Origin of granitic rocks at the southern margin of the Ryoke belt in the Mikawaono-Toei area, central Japan : Rb-Sr dating and tectonic implications
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121-133
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Rb-Sr whole rock isochron ages of granitic rocks from the central Kyushu, Japan
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135-150
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Sedimentary environments and paleogeography of the Lower Cretaceous in South-west Japan based on paleobiogeography of ammonites and dinosaurs
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151-165
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Active ridge-forearc collision and its geological consequences : an example from Late Cretaceous Southwest Japan
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167-182
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Tectonics and sedimentation of the Tertiary sedimentary basins in the northem Kyushu
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183-201
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Formation of the Akaishi Tectonic Zone and its significance on the crustal recontruction of the eastern part of Southwest Japan Arc during the Miocene
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203-223
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Deformation of the forearc region and along the Median Tectonic Line in southwest Japan during the opening of the Japan Sea : A preliminary report
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225-244
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Collision of the Kushigatayama block during the Middle Miocene, northwestern part of South Fossa-Magna, central Japan
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245-254
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Generation of magnesian andesites in the Setouchi region
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255-266
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K-Ar ages and the origin of acidic volcanic rocks along the Median Tectonic Line at northwest Shikoku, Japan
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267-278
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Middle Miocene thermal metamorphism in the Sanbagawa metamorphic belt, western Shikoku, Southwest Japan
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279-296
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Formation of Ishizuchi cauldron and Miocene tectonics
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297-349
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Numerical experiments for recovery of reversed thermal structure in arc-trench system : new constraints on orogenic process
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351-357
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CONTENTS
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裏表紙
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CONTENTS
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