| Title Transcription | ヒルゼン ゲンソウチュウ ニ ハッタツ スル ダンレツ ノ カイセキ
|
| Title Alternative (English) | Faults and Stresses in the Hiruzenbara Formation
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| File | |
| language |
jpn
|
| Author |
Kitagawa, Hiroya
Komuro, Hiroaki
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| Description | Normal faults predominant in the Himzenbara Formation of Pleistocene diatomite indicate extensional stress condition．Many sand veins filling between planes of these faults and some diapirs of massive sandy-diatomite are observed at the central part of a large dome．Stress orientations described by the analyses of conjugate faults are good agreement with structural geometry of this dome．Accordingly，the diapiric doming induced the faulting．This doming may be due to fluidization of sandy diatomite，because flow marks are observed along the diapir margin．Walls of the diapir are also delaminated probably by fluidized sandy diatomite．Moreover，median diameters of the sandy diatomite indicate very fluidizable property．
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| Journal Title |
島根大学地球資源環境学研究報告
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| Volume | 12
|
| Start Page | 35
|
| End Page | 43
|
| ISSN | 13439774
|
| Published Date | 1993-08-30
|
| NCID | AA11455176
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| Publisher | 島根大学総合理工学部地球資源環境学教室
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| Publisher Aalternative | Department of Geoscience, Interdisciplinary Faculty of Science and Engineering, Shimane University
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| NII Type |
Departmental Bulletin Paper
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| OAI-PMH Set |
Interdisciplinary Graduate School of Science and Engineering
|
| Remark | 12-14,16+ / 1993+
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| 他の一覧 |
