PROPERTIES OF RESERVOIR QUALITY ROCKS OF THE BELAIT AND LAMBIR FORMATIONS, NORTH EAST SARAWAK

This studywas conducted to evaluate the field characteristics, mineralogical, physical and geochemical properties of the Early to Late Miocene Belait Formation in Marudi and the Early to Middle Miocene Lambir Formation in Miri, Sarawak at various scales of observations and to provide a key differ...

Full description

Saved in:
Bibliographic Details
Main Author: RAMLI, MOHD SYAMIM
Format: Thesis
Language:English
Published: 2013
Subjects:
Online Access:http://utpedia.utp.edu.my/id/eprint/15290/1/2013%20-Properties%20Of%20Reservoir%20Quality%20Rocks%20Of%20The%20Belait%20%26%20LAmbir%20Formations%20North%20East%20Sarawak.pdf
http://utpedia.utp.edu.my/id/eprint/15290/
Tags: Add Tag
No Tags, Be the first to tag this record!
Institution: Universiti Teknologi Petronas
Language: English
id oai:utpedia.utp.edu.my:15290
record_format eprints
spelling oai:utpedia.utp.edu.my:152902024-07-23T09:38:21Z http://utpedia.utp.edu.my/id/eprint/15290/ PROPERTIES OF RESERVOIR QUALITY ROCKS OF THE BELAIT AND LAMBIR FORMATIONS, NORTH EAST SARAWAK RAMLI, MOHD SYAMIM T Technology (General) This studywas conducted to evaluate the field characteristics, mineralogical, physical and geochemical properties of the Early to Late Miocene Belait Formation in Marudi and the Early to Middle Miocene Lambir Formation in Miri, Sarawak at various scales of observations and to provide a key differentiation between these two formations. Representative samples were collected at Marudi, Northern Sarawak (Belait Formation) and nearby Miri, Sarawak (Lambir Formation). Field observations suggested that there are at least four differentiating characteristics between these Formations. The four major differentiating characteristics are; microfabric analysis revealed that the Belait Formation consists of angular to sub-angular grains whereas the Lambir Formation has sub-rounded grains. Presence of mudclasts in the Belait Formation suggests deposition in a low energy, muddy environment with short transportation. Extensive fracturing of the quartz grains in the Belait Formation suggests variations in the degree of compaction resulting from differences in thickness or rates of diagenesis. 2013-03 Thesis NonPeerReviewed application/pdf en http://utpedia.utp.edu.my/id/eprint/15290/1/2013%20-Properties%20Of%20Reservoir%20Quality%20Rocks%20Of%20The%20Belait%20%26%20LAmbir%20Formations%20North%20East%20Sarawak.pdf RAMLI, MOHD SYAMIM (2013) PROPERTIES OF RESERVOIR QUALITY ROCKS OF THE BELAIT AND LAMBIR FORMATIONS, NORTH EAST SARAWAK. Masters thesis, Universiti Teknologi PETRONAS.
institution Universiti Teknologi Petronas
building UTP Resource Centre
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Teknologi Petronas
content_source UTP Electronic and Digitized Intellectual Asset
url_provider http://utpedia.utp.edu.my/
language English
topic T Technology (General)
spellingShingle T Technology (General)
RAMLI, MOHD SYAMIM
PROPERTIES OF RESERVOIR QUALITY ROCKS OF THE BELAIT AND LAMBIR FORMATIONS, NORTH EAST SARAWAK
description This studywas conducted to evaluate the field characteristics, mineralogical, physical and geochemical properties of the Early to Late Miocene Belait Formation in Marudi and the Early to Middle Miocene Lambir Formation in Miri, Sarawak at various scales of observations and to provide a key differentiation between these two formations. Representative samples were collected at Marudi, Northern Sarawak (Belait Formation) and nearby Miri, Sarawak (Lambir Formation). Field observations suggested that there are at least four differentiating characteristics between these Formations. The four major differentiating characteristics are; microfabric analysis revealed that the Belait Formation consists of angular to sub-angular grains whereas the Lambir Formation has sub-rounded grains. Presence of mudclasts in the Belait Formation suggests deposition in a low energy, muddy environment with short transportation. Extensive fracturing of the quartz grains in the Belait Formation suggests variations in the degree of compaction resulting from differences in thickness or rates of diagenesis.
format Thesis
author RAMLI, MOHD SYAMIM
author_facet RAMLI, MOHD SYAMIM
author_sort RAMLI, MOHD SYAMIM
title PROPERTIES OF RESERVOIR QUALITY ROCKS OF THE BELAIT AND LAMBIR FORMATIONS, NORTH EAST SARAWAK
title_short PROPERTIES OF RESERVOIR QUALITY ROCKS OF THE BELAIT AND LAMBIR FORMATIONS, NORTH EAST SARAWAK
title_full PROPERTIES OF RESERVOIR QUALITY ROCKS OF THE BELAIT AND LAMBIR FORMATIONS, NORTH EAST SARAWAK
title_fullStr PROPERTIES OF RESERVOIR QUALITY ROCKS OF THE BELAIT AND LAMBIR FORMATIONS, NORTH EAST SARAWAK
title_full_unstemmed PROPERTIES OF RESERVOIR QUALITY ROCKS OF THE BELAIT AND LAMBIR FORMATIONS, NORTH EAST SARAWAK
title_sort properties of reservoir quality rocks of the belait and lambir formations, north east sarawak
publishDate 2013
url http://utpedia.utp.edu.my/id/eprint/15290/1/2013%20-Properties%20Of%20Reservoir%20Quality%20Rocks%20Of%20The%20Belait%20%26%20LAmbir%20Formations%20North%20East%20Sarawak.pdf
http://utpedia.utp.edu.my/id/eprint/15290/
_version_ 1805890997689778176