Zobrazeno 1 - 10
of 27
pro vyhledávání: '"Osaka Group"'
Publikováno v:
Earth, Planets and Space, Vol 73, Iss 1, Pp 1-18 (2021)
Abstract The geometries (i.e., dip angles) of active faults from the surface to the seismogenic zone are the most important factors used to evaluate earthquake ground motion, which is crucial for seismic hazard assessments in urban areas. In Osaka, a
Externí odkaz:
https://doaj.org/article/a78297a561bb44718ae42451aada502c
Publikováno v:
大阪市立自然史博物館研究報告 = Bulletin of the Osaka Museum of Natural History. 76:31-55
淡路島北部東岸沖の大阪湾海底から,底曳き網漁に伴い,シカ類,イノシシ類,魚類,そして淡水貝類を含む,多くの種類の化石が引き上げられており,その年代は軟体動物の生層序,
Publikováno v:
Earth, Planets and Space, Vol 73, Iss 1, Pp 1-18 (2021)
The geometries (i.e., dip angles) of active faults from the surface to the seismogenic zone are the most important factors used to evaluate earthquake ground motion, which is crucial for seismic hazard assessments in urban areas. In Osaka, a metropol
Akademický článek
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Akademický článek
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Publikováno v:
日本地すべり学会誌 : 地すべり. 44(4):214-221
Autor:
Muslim, Dicky
Publikováno v:
Journal of geosciences Osaka City University. 45:63-71
The Sennan Formation, the Lowermost part of the Quaternary Osaka Group, is composed of inter-calations of unconsolidated gravel, sand and silt, and is distributed in the southern margin of the basin. In this formation, faults are expressed as tectoni
Autor:
Hiraoka, Yoshihiro
Publikováno v:
Journal of geosciences Osaka City University. 41:1-17
The origin of sediments of the Pliocene and Pleistocene Osaka Group was estimated on the basis of chemical analysis of detrital biotite. Samples examined were biotite crystals of granitoid gravels, sands and silts collected from the Uji hills, the Ke
Publikováno v:
島根大学地球資源環境学研究報告. 15:47-52
Many pollen stratigraphy from Pliocene-Pleistocene sediments have been studied in Western Honshu,Japan. Recently stragraphy of the sediments in many area has been revised by correlation of volcanic ash layers. In this paper,pollen flora are exami
Publikováno v:
愛知教育大学研究報告. 自然科学. 43:51-68
Kawamura (1993) described the detailed stratigraphy of the Plio-Pleistocene Osaka Group in the Nara Hills. Additional data to the paper are given here to discuss the relationships to previous works (Yokoyama and Nakagawa, 1984; Mitamura, 1992 etc.) T