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DCフィールド | 値 | 言語 |
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dc.contributor.author | Hattori, Tomoo | en |
dc.contributor.alternative | 服部, 共生 | ja |
dc.contributor.transcription | ハットリ, トモオ | ja-Kana |
dc.date.accessioned | 2008-05-15T04:23:42Z | - |
dc.date.available | 2008-05-15T04:23:42Z | - |
dc.date.issued | 1972-09 | - |
dc.identifier.issn | 0563-8682 | - |
dc.identifier.uri | http://hdl.handle.net/2433/55703 | - |
dc.description | この論文は国立情報学研究所の学術雑誌公開支援事業により電子化されました。 | ja |
dc.description.abstract | The author has been done stratigraphical studies of Quaternary sediments of the Chao Phraya drainage basin using chemical and mineralogical methods. The results for the uppermost streams (the Lampang basin), the middle stream and the near-apex area of the deltaic part of the basin have already been published. The present paper deals with the near-gulf part of the delta. In the areas reported in the preceding papers, it was the main target to make clear the relationship between weathering intensity and stratigraphical position. Whereas in this paper, the relation between the chemical properties of sediments and its depositional environment is tested as the main topics, since the area is dominated by recent sediments whose properties are more strongly controlled by depositional condition rather than the deteriolation by weathering. | en |
dc.language.iso | eng | - |
dc.publisher | 京都大学東南アジア研究センター | ja |
dc.publisher.alternative | Center for Southeast Asian Studies, Kyoto University | en |
dc.subject.ndc | 292.3 | - |
dc.title | <Notes>Some Properties of Recent Sediments in the Bangkok Plain of Thailand | en |
dc.type | departmental bulletin paper | - |
dc.type.niitype | Departmental Bulletin Paper | - |
dc.identifier.ncid | AN00166463 | - |
dc.identifier.jtitle | 東南アジア研究 | ja |
dc.identifier.volume | 10 | - |
dc.identifier.issue | 2 | - |
dc.identifier.spage | 321 | - |
dc.identifier.epage | 334 | - |
dc.textversion | publisher | - |
dc.sortkey | 13 | - |
dcterms.accessRights | open access | - |
dc.identifier.pissn | 0563-8682 | - |
出現コレクション: | Vol.10 No.2 |
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