Open AccessJournal Article
Quaternary Geology of Osaka wiht Special Reference to Land Subsidence
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This article is published in Journal of geosciences, Osaka City University.The article was published on 1970-03-01 and is currently open access. It has received 48 citations till now.read more
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Magnetostratigraphy of Plio-Pleistocene sediments in a 1700-m core from Osaka Bay, southwestern Japan and short geomagnetic events in the middle Matuyama and early Brunhes chrons
D.K Biswas,Masayuki Hyodo,Y Taniguchi,Masanori Kaneko,Shigehiro Katoh,Hiroshi Sato,Y Kinugasa,K Mizuno +7 more
TL;DR: A magnetic polarity stratigraphy spanning more than the past 3.2 Myr was determined for a long 1545 m continuous sedimentary sequence of marine, fluvial, and lacustrine deposits from the Osaka Basin, southwestern Japan as discussed by the authors.
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Basin-Induced Love Waves in the Eastern Part of the Osaka Basin.
TL;DR: In this article, a basin-induced Love wave was detected as later arrivals of a direct S-wave in seismograms observed in the Osaka basin located in western Honshu, Japan from three deep earthquakes occurring near Japan.
Journal Article
Basin-Induced Love Waves in the Eastern Part of the Osaka Basin.
TL;DR: In this paper, a basin-induced Love wave was detected as later arrivals of a direct S-wave in seismograms observed in the Osaka basin located in western Honshu, Japan from three deep earthquakes occurring near Japan.
Journal ArticleDOI
Stratigraphy and Correlation of the Plio-Pleistocene Volcanic Ash Layers from a 1, 700m Core Taken from Higashinada, Kobe City, Southwestern Japan
Shusaku Yoshikawa,Kiyohide Mizuno,Shigehiro Katoh,Yasufumi Satoguchi,Chihiro Miyakawa,Yoshihiro Kinugasa,Muneki Mitamura,Koichi Nakagawa +7 more
TL;DR: K1-L 1,545.7m as discussed by the authors (1,705.8m) was the best performance of K1-U 1,068.3m.
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Basin formation at a contractional bend of a large transcurrent fault: Plio-Pleistocene subsidence of the Kobe and northern Osaka Basins, Japan
TL;DR: In this article, the authors studied the basin formation process at a contractional bend of a large transcurrent fault from the viewpoint of extensive subsidence history, where the Kobe and northern Osaka basins in southwest Japan are located at the easternmost left-stepping bend of the dextral Median Tectonic Line (MTL), a fault system activated throughout the Quaternary.