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mfskugm 034001_023.pdf | 1.8 MB | Adobe PDF | 見る/開く |
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DCフィールド | 値 | 言語 |
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dc.contributor.author | Terashima, Hideshi | en |
dc.contributor.alternative | テラシマ, ヒデシ | ja |
dc.contributor.transcription | テラシマ, ヒデシ | ja-Kana |
dc.date.accessioned | 2014-05-01T05:39:03Z | - |
dc.date.available | 2014-05-01T05:39:03Z | - |
dc.date.issued | 1967-12-16 | - |
dc.identifier.issn | 0454-7810 | - |
dc.identifier.uri | http://hdl.handle.net/2433/186541 | - |
dc.description.abstract | In the Paleogene rocks of the Muroto district sandstone dikes are found in many localities. They occur invariably within shaly flysch-type rocks and not essentially associated with slumping. The material of the dikes was filled into fissures from above and/or below. In addition the paper deals with the origin of the dikes and their deformation. Fissuring in the desposits was probably caused by an underwater earthquake. The sandstone dikes show not only ptygmatic folding by the compaction of the surrounding rocks, but also are folded, faulted, and fractured through later orogenic movements, depending on their initial attitude. | en |
dc.format.mimetype | application/pdf | - |
dc.language.iso | eng | - |
dc.publisher | 京都大学理学部 | ja |
dc.publisher.alternative | [Faculty of Science, Kyoto University] | en |
dc.subject.ndc | 450 | - |
dc.title | On the Paleogene Sandstone Dikes in the Muroto District, Shikoku Island, Southwest Japan | en |
dc.type | departmental bulletin paper | - |
dc.type.niitype | Departmental Bulletin Paper | - |
dc.identifier.ncid | AA00732831 | - |
dc.identifier.jtitle | Memoirs of the Faculty of Science, Kyoto University. Series of geology and mineralogy | en |
dc.identifier.volume | 34 | - |
dc.identifier.issue | 1 | - |
dc.identifier.spage | 23 | - |
dc.identifier.epage | 34 | - |
dc.textversion | publisher | - |
dc.sortkey | 04 | - |
dc.address | Geological and Mineralogical Institute, Kyoto University | en |
dcterms.accessRights | open access | - |
dc.identifier.pissn | 0454-7810 | - |
出現コレクション: | Vol. 34 No. 1 |
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