SEDIMENTOLOGY AND STRATIGRAPHY (BIOSTRATIGRAPHY) OF THE KAYAN SANDSTONE FORMATION, LUNDU AREA, SARAWAK – TRANSECT II

This project presents detailed sedimentology and stratigraphy of the Kayan Sandstone Formation (Upper Cretaceous to Middle Miocene) exposed along the Bau-Lundu Road, Sarawak. The present work on the Kayan Sandstone Formation is based on previous research and current work. Field investigation, doc...

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Main Author: BIN AZMAN, ALI IMRAN
Format: Final Year Project
Language:English
Published: Universiti Teknologi PETRONAS 2015
Subjects:
Online Access:http://utpedia.utp.edu.my/18182/1/Dissertation.pdf
http://utpedia.utp.edu.my/18182/
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spelling my-utp-utpedia.181822018-11-22T14:39:47Z http://utpedia.utp.edu.my/18182/ SEDIMENTOLOGY AND STRATIGRAPHY (BIOSTRATIGRAPHY) OF THE KAYAN SANDSTONE FORMATION, LUNDU AREA, SARAWAK – TRANSECT II BIN AZMAN, ALI IMRAN G Geography (General) This project presents detailed sedimentology and stratigraphy of the Kayan Sandstone Formation (Upper Cretaceous to Middle Miocene) exposed along the Bau-Lundu Road, Sarawak. The present work on the Kayan Sandstone Formation is based on previous research and current work. Field investigation, documentation and sample collection were carried out in the Lundu area near Kuching, Sarawak. Samples collected were analyzed for thin section and grain size analysis in the laboratory at Universiti Teknologi PETRONAS (UTP) and palynology analysis at Biostratex Sdn. Bhd. Four types of sedimentary facies were recognized within the Kayan Sandstone Formation. Sedimentary facies identified are i) Trough cross bedding sandstone; ii) Planar cross bedding sandstone; iii) Interbedded sandstone-mudstone; and iv) Massive mudstone. From the facies analysis, three facies associations were recognized, which are i) Planar and trough cross bedding sandstone interbedded with thin mudstone; ii) Planar cross bedding sandstone interbedded with pebbles; and iii) Thick massive sandstone. Based on the facies association and laboratory analyses, the Kayan Sandstone Formation can be interpreted that the sandstones are typically of fluvial environment. Universiti Teknologi PETRONAS 2015-09 Final Year Project NonPeerReviewed application/pdf en http://utpedia.utp.edu.my/18182/1/Dissertation.pdf BIN AZMAN, ALI IMRAN (2015) SEDIMENTOLOGY AND STRATIGRAPHY (BIOSTRATIGRAPHY) OF THE KAYAN SANDSTONE FORMATION, LUNDU AREA, SARAWAK – TRANSECT II. Universiti Teknologi PETRONAS. (Submitted)
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 G Geography (General)
spellingShingle G Geography (General)
BIN AZMAN, ALI IMRAN
SEDIMENTOLOGY AND STRATIGRAPHY (BIOSTRATIGRAPHY) OF THE KAYAN SANDSTONE FORMATION, LUNDU AREA, SARAWAK – TRANSECT II
description This project presents detailed sedimentology and stratigraphy of the Kayan Sandstone Formation (Upper Cretaceous to Middle Miocene) exposed along the Bau-Lundu Road, Sarawak. The present work on the Kayan Sandstone Formation is based on previous research and current work. Field investigation, documentation and sample collection were carried out in the Lundu area near Kuching, Sarawak. Samples collected were analyzed for thin section and grain size analysis in the laboratory at Universiti Teknologi PETRONAS (UTP) and palynology analysis at Biostratex Sdn. Bhd. Four types of sedimentary facies were recognized within the Kayan Sandstone Formation. Sedimentary facies identified are i) Trough cross bedding sandstone; ii) Planar cross bedding sandstone; iii) Interbedded sandstone-mudstone; and iv) Massive mudstone. From the facies analysis, three facies associations were recognized, which are i) Planar and trough cross bedding sandstone interbedded with thin mudstone; ii) Planar cross bedding sandstone interbedded with pebbles; and iii) Thick massive sandstone. Based on the facies association and laboratory analyses, the Kayan Sandstone Formation can be interpreted that the sandstones are typically of fluvial environment.
format Final Year Project
author BIN AZMAN, ALI IMRAN
author_facet BIN AZMAN, ALI IMRAN
author_sort BIN AZMAN, ALI IMRAN
title SEDIMENTOLOGY AND STRATIGRAPHY (BIOSTRATIGRAPHY) OF THE KAYAN SANDSTONE FORMATION, LUNDU AREA, SARAWAK – TRANSECT II
title_short SEDIMENTOLOGY AND STRATIGRAPHY (BIOSTRATIGRAPHY) OF THE KAYAN SANDSTONE FORMATION, LUNDU AREA, SARAWAK – TRANSECT II
title_full SEDIMENTOLOGY AND STRATIGRAPHY (BIOSTRATIGRAPHY) OF THE KAYAN SANDSTONE FORMATION, LUNDU AREA, SARAWAK – TRANSECT II
title_fullStr SEDIMENTOLOGY AND STRATIGRAPHY (BIOSTRATIGRAPHY) OF THE KAYAN SANDSTONE FORMATION, LUNDU AREA, SARAWAK – TRANSECT II
title_full_unstemmed SEDIMENTOLOGY AND STRATIGRAPHY (BIOSTRATIGRAPHY) OF THE KAYAN SANDSTONE FORMATION, LUNDU AREA, SARAWAK – TRANSECT II
title_sort sedimentology and stratigraphy (biostratigraphy) of the kayan sandstone formation, lundu area, sarawak – transect ii
publisher Universiti Teknologi PETRONAS
publishDate 2015
url http://utpedia.utp.edu.my/18182/1/Dissertation.pdf
http://utpedia.utp.edu.my/18182/
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score 13.188404