Please use this identifier to cite or link to this item: https://ptsldigital.ukm.my/jspui/handle/123456789/776149
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dc.contributor.authorSin Sinsikul-
dc.date.accessioned2024-10-01T03:31:19Z-
dc.date.available2024-10-01T03:31:19Z-
dc.identifier.isbn974-7809-20-6en_US
dc.identifier.urihttps://ptsldigital.ukm.my/jspui/handle/123456789/776149-
dc.description.abstractThere are interactions between archaeology and geology, particularly in the Quaternary period. Geomorphologic, stratigraphic and lithologic evidences are used to decipher the Quaternary environmental changes and level event in the coastal areas of Phangnga and Krabi. sea The data suggest that relative rise in sea level up to 5,700 B.P., with height of 4.5 metres above local mean This has an important effect on landform development.en_US
dc.language.isoenen_US
dc.publisherSPAFA Co-ordinating Uniten_US
dc.subjectGeomorphologyen_US
dc.subjectArchaeologyen_US
dc.subjectSea levelen_US
dc.titleQuaternary geology and sea-level changes in the area of phangnga and krabi: implications for prehistoric archaeologyen_US
dc.typeSeminar Papersen_US
dc.format.pages313-322en_US
dc.identifier.callnoDS525.S45 1987 katsemen_US
dc.contributor.conferencenameSeminar in Prehistory of Southeast Asia [T-W11]-
dc.coverage.conferencelocationBangkok, Thailand-
dc.date.conferencedate1987-12-12-
Appears in Collections:Seminar Papers/ Proceedings / Kertas Kerja Seminar/ Prosiding

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