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dc.contributor.authorMd Mostafizur Rahman-
dc.date.accessioned2018-02-01T00:34:35Z-
dc.date.available2018-02-01T00:34:35Z-
dc.date.issued2016-
dc.identifier.urihttp://hdl.handle.net/123456789/8216-
dc.description.abstractValley incision and infilling, as well as the fluvial response of uppermost Pilong formation in Penyu Basin located offshore of present-day Pahang River Basin, Peninsular Malaysia during Late Pleistocene-Mid Holocene was studied. A detailed study of time slices, horizon surfaces and vertical sections of three-dimensional (3D) volume data, high-resolution two-dimensional (2D) CHIRP acoustic profiles, and seabed bathymetric data provided a very good opportunity to delineate the changes of the deglacial fluvial pattern as well as its internal morphology and its evolution through geologic time. Based on the fluvial origin, plan-view pattern and internal architecture, six classes of deglacial fluvial sequences have been categorized.en_US
dc.language.isoenen_US
dc.publisherTerengganu: Universiti Malaysia Terengganuen_US
dc.subjectQE 571 .M3 2016en_US
dc.subjectMd Mostafizur Rahmanen_US
dc.subjectSedimentation and depositionen_US
dc.subjectValleysen_US
dc.titleResponse of incised valley systems with sea level change during late pleistocene-holocene at Penyu Basin, Sunda Shelfen_US
dc.typeThesisen_US
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