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- W2809707486 abstract "This chapter briefly describes the stratigraphic basis of the Osaka Group, which has been accumulating within the Osaka sedimentary basin since ca. 3.5 Ma. Among the three Plio-Pleistocene basins in the Kinki district of southwest Japan (Tokai, Paleo-Lake Biwa, and Osaka), the Osaka basin, which has a wide aperture connecting the inlet and the open sea, shows the largest diversity in sedimentary environments (fluvial, lacustrine, tidal, and deltaic) as a result of the influence of eustatic sea-level changes and the tectonic deformation of the crust of the island arc. This chapter provides an overview of the biostratigraphy, magnetostratigraphy, and tephrochronology of the event sediments, which are then used to reconstruct a detailed paleogeographic description of the study area during recent periods. Then, the results of deep drilling surveys are described to cultivate a fundamental notion of the evolutionary processes of the basin. Finally, tectonic movements are evaluated quantitatively from the burial histories of select boreholes, which have been finely tuned based on the oxygen isotope stage boundaries. The interval subsidence rates through the late Quaternary were calculated based on subsurface datum levels in the Osaka Group. The results revealed that the differential subsidence of the basement was likely controlled by changes in the tectonic stress regime related to the transient mode of oceanic plate convergence." @default.
- W2809707486 created "2018-07-10" @default.
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- W2809707486 date "2018-05-31" @default.
- W2809707486 modified "2023-09-25" @default.
- W2809707486 title "Basic Knowledge—Stratigraphy of the Osaka Group" @default.
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- W2809707486 doi "https://doi.org/10.1007/978-981-13-0577-1_2" @default.
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