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THE HOLOCENE-TO-RECENT GEOMORPHOLOGICAL, SEDIMENTOLOGICAL AND STRATIGRAPHIC DEVELOPMENT OF THE LOWER PERAK RIVER AND ITS COASTAL-DELTAIC PLAIN

ABD. MANAF, MAIZATUL ASNIDA (2015) THE HOLOCENE-TO-RECENT GEOMORPHOLOGICAL, SEDIMENTOLOGICAL AND STRATIGRAPHIC DEVELOPMENT OF THE LOWER PERAK RIVER AND ITS COASTAL-DELTAIC PLAIN. Masters thesis, Universiti Teknologi PETRONAS.

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Abstract

This study focuses on the geomorphology, sedimentology and stratigraphy of lower Perak coastal deltaic-plain in relation to Holocene sea level change. The Perak River is located on the west flank of Peninsular Malaysia and can be divided into four geographic regions; lower and upper parts for both of the upstream and coastal areas. The channel pattern occurred in this area includes the straight-braided and meandering. The river flow changes it direction from north to south before drifted easterly to the west at Teluk Intan.

Item Type: Thesis (Masters)
Academic Subject : Academic Department - Petroleum Geosciences - Petrophysics - Petrophysical data acquisition
Subject: Q Science > QE Geology
Divisions: Geoscience and Petroleum Engineering
Depositing User: Ahmad Suhairi Mohamed Lazim
Date Deposited: 02 Oct 2019 14:24
Last Modified: 02 Oct 2019 14:24
URI: http://utpedia.utp.edu.my/id/eprint/19980

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