A new interpretation of forming process of marine pleistocene succession in the kanto tectonic basin

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概要

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• Relatively thick marine Pleistocene deposits, the Kazusa and the Shimosa Groups. are exposed in the Boso Peninsula, central Japan. It is generally said that the continuous tectonic subsidence of the Kanto Tectonic Basin causes such remarkable sedimentation. Especially the Shimosa Group consists of a succession of several formations controlled by glacio-eustasy. Besides, the Basin must have upheaved from deep sea during the Quaternary, because it is located on the wide uplift belt of the island arc. Owing to interpretation of the paradox, two hypothetical ideas are proposed: one is related to tectono-eustatic sea-level rise, and the other is isostatic subsidence caused by sediment loading. The next idea is superposition of both processes.

• 首都大学東京の論文

著者

• Kikuchi Takao

  Department Of Geography Tokyo Metropolitan University

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• A new interpretation of forming process of marine pleistocene succession in the kanto tectonic basin
• Optical Birefringence Measurements in Ferromagnetic and Antiferromagnetic Alternating Heisenberg Chains (CH3)2CHNH3CuCl3

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