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Development of the Cretaceous Sedimentary Basin of the Sanchu Graben, Kanto Mountains, Japan

Kensaku Takei

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Abstract

The Sanchu Graben of the Kanto Mountains is one of the Cretaceous basins of the Chichibu Belt, but is unique in its tectonic position that it is located at the eastern wing of the syntaxis structure against the other basins which form the western wing. The Cretaceous strata in the Sanchu Graben are composed of marine and partly brackish sediments and form synclinal structures....

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The Sanchu Graben of the Kanto Mountains is one of the Cretaceous basins of the Chichibu Belt, but is unique in its tectonic position that it is located at the eastern wing of the syntaxis structure against the other basins which form the western wing. The Cretaceous strata in the Sanchu Graben are composed of marine and partly brackish sediments and form synclinal structures....

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Available abstract

The Sanchu Graben of the Kanto Mountains is one of the Cretaceous basins of the Chichibu Belt, but is unique in its tectonic position that it is located at the eastern wing of the syntaxis structure against the other basins which form the western wing. The Cretaceous strata in the Sanchu Graben are composed of marine and partly brackish sediments and form synclinal structures....

Key concepts: Graben, Geology, Cretaceous, Structural basin, Sedimentary rock, Paleontology, Geomorphology

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Development of the Cretaceous Sedimentary Basin of the Sanchu Graben, Kanto Mountains, Japan — Research Paper | ScholarLens