Please use this identifier to cite or link to this item: http://umt-ir.umt.edu.my:8080/handle/123456789/8216
Title: Response of incised valley systems with sea level change during late pleistocene-holocene at Penyu Basin, Sunda Shelf
Authors: Md Mostafizur Rahman
Keywords: QE 571 .M3 2016
Md Mostafizur Rahman
Sedimentation and deposition
Valleys
Issue Date: 2016
Publisher: Terengganu: Universiti Malaysia Terengganu
Abstract: Valley 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.
URI: http://hdl.handle.net/123456789/8216
Appears in Collections:Pusat Pengajian Sains Marin Dan Sekitaran

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