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dc.contributor.authorHattori, Tomooen
dc.contributor.alternative服部, 共生ja
dc.contributor.transcriptionハットリ, トモオja-Kana
dc.date.accessioned2008-05-15T04:23:42Z-
dc.date.available2008-05-15T04:23:42Z-
dc.date.issued1972-09-
dc.identifier.issn0563-8682-
dc.identifier.urihttp://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.abstractThe 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.isoeng-
dc.publisher京都大学東南アジア研究センターja
dc.publisher.alternativeCenter for Southeast Asian Studies, Kyoto Universityen
dc.subject.ndc292.3-
dc.title<Notes>Some Properties of Recent Sediments in the Bangkok Plain of Thailanden
dc.typedepartmental bulletin paper-
dc.type.niitypeDepartmental Bulletin Paper-
dc.identifier.ncidAN00166463-
dc.identifier.jtitle東南アジア研究ja
dc.identifier.volume10-
dc.identifier.issue2-
dc.identifier.spage321-
dc.identifier.epage334-
dc.textversionpublisher-
dc.sortkey13-
dcterms.accessRightsopen access-
dc.identifier.pissn0563-8682-
出現コレクション:Vol.10 No.2

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