DIAGENETIC HISTORY OF CARBONATES IN EAST SABAH

During Oligocene – Miocene, there is a major tectonic deformation which cause a widespread of uplift followed by carbonate sedimentation (Gomantong Limestone Formation) when the depositional environment changed from deep to shallow marine. These onshore Gomantong Limestone formations are often is...

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Bibliographic Details

Main Author:	RAYMOND, ROZEN REVILENE
Format:	Final Year Project
Language:	en
Published:	Universiti Teknologi PETRONAS 2015
Subjects:	G Geography (General)
Online Access:	http://utpedia.utp.edu.my/id/eprint/18191/1/1.%20Dissertations%20-%20ROZEN%2015302.pdf http://utpedia.utp.edu.my/id/eprint/18191/
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