Opening of Japan Sea and Major Tectonic Lines of Japan

修一, 柳井; 一勝, 青木; 良光, 赤堀

doi:10.5026/jgeography.119.1079

Cited by 66 publications

(28 citation statements)

References 64 publications

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“…The subsequent strike-slip movement of Neo-MTL occurred later when the Nanakai fore-arc sliver became activated. For further details of the opening of the Japan Sea, refer to Tamaki (1985), Otofuji and Matsuda (1987), Jolivert et al (1994) and Yanai et al (2010).…”

Section: Spatial Arrangement Of Orogenic Componentsmentioning

confidence: 99%

Recognition of the Shimanto HP metamorphic belt within the traditional Sanbagawa HP metamorphic belt: New perspectives of the Cretaceous–Paleogene tectonics in Japan

Aoki

Maruyama

Isozaki

et al. 2011

Journal of Asian Earth Sciences

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Section: Spatial Arrangement Of Orogenic Componentsmentioning

confidence: 99%

Recognition of the Shimanto HP metamorphic belt within the traditional Sanbagawa HP metamorphic belt: New perspectives of the Cretaceous–Paleogene tectonics in Japan

Aoki

Maruyama

Isozaki

et al. 2011

Journal of Asian Earth Sciences

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“…Several scientists think that it extends to the north-west, to the Sikhote-Alin Mountains in Russian Far East Safonova et al, 2009;Yanai et al, 2010). This AC is composed of accreted Carboniferous-Permian basalts and limestones and Permian-Jurassic cherts ( Fig.…”

mentioning

confidence: 98%

Recognizing OIB and MORB in accretionary complexes: A new approach based on ocean plate stratigraphy, petrology and geochemistry

et al. 2016

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“…It was formed behind the Japanese island‐arc system initiated by the rifting of the eastern margin of the Eurasian Continent at around 25 to 20 Ma (Tamaki ; Tamaki & Isezaki ; Yanai et al . ). The opening of the Japan Sea was only a short event, which was almost completed before 15 Ma (Otofuji et al .…”

Section: Methodsmentioning

confidence: 97%

Correlating biostratigraphy and palaeoceanographic changes during late Quaternary at cold seeps with gas hydrate‐free areas of the Japan Sea using foraminifera paleoecology

et al. 2016

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Late Quaternary foraminifera assemblages have been examined in two sediment cores (MD179‐3296 and MD179‐3317) from cold seep areas in the eastern margin of the Japan Sea, off Joetsu, Niigata Prefecture. Foraminifera assemblages in core MD179‐3296, which was located at the center of a pockmark on the Umitake Spur, show no evidence of methane flux and, especially in its upper portion, share the same paleo‐environmental history as other free gas hydrate areas of the Japan Sea. In comparison, in the core MD179‐3317 at the center of a pockmark at Joetsu Knoll, foraminiferal distributions were strongly affected by methane activities and, in the main part of the core, were deposited under local conditions. Three horizons were identified in this core, which are characterized by the high abundance value of Thalmannammina parkerae and might be related to methane flux due to sea level fall especially through late marine isotope stage (MIS) 3 and MIS 2.

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Opening of Japan Sea and Major Tectonic Lines of Japan

Cited by 66 publications

References 64 publications

Recognition of the Shimanto HP metamorphic belt within the traditional Sanbagawa HP metamorphic belt: New perspectives of the Cretaceous–Paleogene tectonics in Japan

Recognition of the Shimanto HP metamorphic belt within the traditional Sanbagawa HP metamorphic belt: New perspectives of the Cretaceous–Paleogene tectonics in Japan

Recognizing OIB and MORB in accretionary complexes: A new approach based on ocean plate stratigraphy, petrology and geochemistry

Correlating biostratigraphy and palaeoceanographic changes during late Quaternary at cold seeps with gas hydrate‐free areas of the Japan Sea using foraminifera paleoecology

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