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:English
Published: Universiti Teknologi PETRONAS 2015
Subjects:
Online Access:http://utpedia.utp.edu.my/18191/1/1.%20Dissertations%20-%20ROZEN%2015302.pdf
http://utpedia.utp.edu.my/18191/
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