Zobrazeno 1 - 10
of 23
pro vyhledávání: '"Arata Sugimura"'
Excavation Study of the Kitatake Active Fault at Nagasawa, Yokosuka City, Kanagawa Prefecture, Japan
Autor:
Arata Sugimura, Yasutaka Ikeda, Yoshihito Fujii, Yasumitsu Kanie, Masami Togo, Shigeo Asami, Masaru Saito, Yoko Ota, Hiroshi Sato, Tetsuto Eto
Publikováno v:
Journal of Geography (Chigaku Zasshi). 108:562-588
The Kitatake fault is the major fault of Kitatake fault zone, WNW-ESE striking across the Miura Peninsula, south of Tokyo. The Kitatake fault zone is almost parallel to Kinugasa fault zone (north) and to Takeyama fault zone (south). All of these faul
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::38876164cd5bcc3e34f968001fa79048
https://doi.org/10.5026/jgeography.108.5_562
https://doi.org/10.5026/jgeography.108.5_562
Autor:
Hajime Kayanne, Takao Miyata, Peter Rodda, Arata Sugimura, Yoshiaki Matsushima, Eiji Matsumoto, Yasuo Maeda
Publikováno v:
Quaternary Research. 33:352-359
Two distinct elevations of emerged notches can be recognized on the southeastern coast of Vanua Levu: the higher notch is +2.22 to +3.30 m above low-tide level and the lower +1.52 to +1.65 m above low-tide level. Many emerged Holocene corals encrust
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a867795fbe605e37068828aa6b0b6968
https://doi.org/10.1016/0033-5894(90)90061-o
https://doi.org/10.1016/0033-5894(90)90061-o
Autor:
Arata Sugimura
Publikováno v:
World Regional Geology
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fceb8d4165f61bd284b2ae32a825ce64
https://doi.org/10.1007/3-540-31081-1_63
https://doi.org/10.1007/3-540-31081-1_63
Autor:
Yasutaka Ikeda, Masami Togo, Masaru Saito, Hiroshi Sato, Yasumitsu Kanie, Yoshihito Fujii, Tetsuto Eto, Yoko Ota, Arata Sugimura, Shigeo Asami
Publikováno v:
Journal of Geography (Chigaku Zasshi). 108:Plate5-Plate7
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7e88db1d410be704dcf6c2108e19cb14
https://doi.org/10.5026/jgeography.108.5_plate5
https://doi.org/10.5026/jgeography.108.5_plate5
Publikováno v:
Tectonophysics. 23:427-433
Radiocarbon dates of fifteen samples representing raised shorelines on various islands of the tectonically mobile region of eastern Indonesia suggest rates of tectonic uplift ranging up to 12.5 mm/year. Low rates of 0.35–1.2 mm/year are from Biak I
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a2042255d1db1cafc110373c5538ef51
https://doi.org/10.1016/0040-1951(74)90079-1
https://doi.org/10.1016/0040-1951(74)90079-1
Publikováno v:
Bulletin of Volcanology. 26:125-140
The late Cenozoic orogeny in Japan is briefly reviewed. Amounts of volcanic materials in the three periods of the orogeny are estimated at: early Neogene 150 × 103 km3 (mafic 40 %, salic 60 %), middle and late Neogene 20 × 103 km3 (mafic 70 %, sali
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9c3ed4eb3efcdc4549442f2a62301fc9
https://doi.org/10.1007/bf02597281
https://doi.org/10.1007/bf02597281
Autor:
Arata Sugimura
Publikováno v:
The Journal of the Geological Society of Japan. 67:292-300
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::14126c49ef976641213bb13745a0bfc0
https://doi.org/10.5575/geosoc.67.292
https://doi.org/10.5575/geosoc.67.292
Publikováno v:
The Quaternary Research (Daiyonki-Kenkyu). 10:81-91
Minami-Shitaura fault is an almost vertical fault and 60km south of Tokyo, trending WNW to ESE across the Miura Peninsula. The upper Miocene Hatsuse formation shows a flexure along the fault, in which the southern side of the fault subsided about 500
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fddca18bd20f3dd0bedc297d3f06cc8b
https://doi.org/10.4116/jaqua.10.81
https://doi.org/10.4116/jaqua.10.81
Autor:
Arata Sugimura
Publikováno v:
Geographical Review of Japan. 23:10-16
This paper discusses some geomorphic and geologic features near Tokyo as the result of lowered sea level accompanying the maximum glaciation during the fourth glacial age.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ebf53190b9ab0d58239c37fcd72036c7
https://doi.org/10.4157/grj.23.10
https://doi.org/10.4157/grj.23.10
Autor:
Arata Sugimura
Publikováno v:
The Quaternary Research (Daiyonki-Kenkyu). 2:220-231
The Yanagase fault can be traced 55 kilometers as the northeastern limit of the Biwa Lake basin.1) There are fault-line valleys that follow the line of the fault. It has been inferred that the fault is of recent origin on the basis of geomorphologica
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2d3e86583feedce0b1a48b50e8f48a49
https://doi.org/10.4116/jaqua.2.220
https://doi.org/10.4116/jaqua.2.220