SEDIMENTOLOGY AND PETROGRAPHIC STUDIES OF WEST CROCKER FORMATION IN SULAMAN AREA, KOTA KINABALU, SABAH.
In this paper, the author describes the sedimentology and petrography of West Crocker Formation in Sulaman area, Kota Kinabalu, Sabah. West Crocker Formation is part of the accretionary complex in NW Sabah. The beddings are almost vertical and the sediments are all clastic. The facies in West Crocke...
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Universiti Teknologi PETRONAS
2014
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my-utp-utpedia.182922018-11-22T14:42:10Z http://utpedia.utp.edu.my/18292/ SEDIMENTOLOGY AND PETROGRAPHIC STUDIES OF WEST CROCKER FORMATION IN SULAMAN AREA, KOTA KINABALU, SABAH. Bin Zaini , Hazim Irsyad G Geography (General) In this paper, the author describes the sedimentology and petrography of West Crocker Formation in Sulaman area, Kota Kinabalu, Sabah. West Crocker Formation is part of the accretionary complex in NW Sabah. The beddings are almost vertical and the sediments are all clastic. The facies in West Crocker Formation could be divided into four main groups; i) massive sandstone, ii) silty sandstone, iii) laminated mudstone, ix) carbonaceous shale. The contact between facies shows two main current trends which are strong turbidity current and weak turbidity current. Universiti Teknologi PETRONAS 2014-05 Final Year Project NonPeerReviewed application/pdf en http://utpedia.utp.edu.my/18292/1/Final%20report.pdf Bin Zaini , Hazim Irsyad (2014) SEDIMENTOLOGY AND PETROGRAPHIC STUDIES OF WEST CROCKER FORMATION IN SULAMAN AREA, KOTA KINABALU, SABAH. Universiti Teknologi PETRONAS. (Submitted) |
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G Geography (General) Bin Zaini , Hazim Irsyad SEDIMENTOLOGY AND PETROGRAPHIC STUDIES OF WEST CROCKER FORMATION IN SULAMAN AREA, KOTA KINABALU, SABAH. |
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In this paper, the author describes the sedimentology and petrography of West Crocker Formation in Sulaman area, Kota Kinabalu, Sabah. West Crocker Formation is part of the accretionary complex in NW Sabah. The beddings are almost vertical and the sediments are all clastic. The facies in West Crocker Formation could be divided into four main groups; i) massive sandstone, ii) silty sandstone, iii) laminated mudstone, ix) carbonaceous shale. The contact between facies shows two main current trends which are strong turbidity current and weak turbidity current. |
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Final Year Project |
author |
Bin Zaini , Hazim Irsyad |
author_facet |
Bin Zaini , Hazim Irsyad |
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Bin Zaini , Hazim Irsyad |
title |
SEDIMENTOLOGY AND PETROGRAPHIC STUDIES OF WEST CROCKER FORMATION IN SULAMAN AREA, KOTA KINABALU, SABAH.
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title_short |
SEDIMENTOLOGY AND PETROGRAPHIC STUDIES OF WEST CROCKER FORMATION IN SULAMAN AREA, KOTA KINABALU, SABAH.
|
title_full |
SEDIMENTOLOGY AND PETROGRAPHIC STUDIES OF WEST CROCKER FORMATION IN SULAMAN AREA, KOTA KINABALU, SABAH.
|
title_fullStr |
SEDIMENTOLOGY AND PETROGRAPHIC STUDIES OF WEST CROCKER FORMATION IN SULAMAN AREA, KOTA KINABALU, SABAH.
|
title_full_unstemmed |
SEDIMENTOLOGY AND PETROGRAPHIC STUDIES OF WEST CROCKER FORMATION IN SULAMAN AREA, KOTA KINABALU, SABAH.
|
title_sort |
sedimentology and petrographic studies of west crocker formation in sulaman area, kota kinabalu, sabah. |
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Universiti Teknologi PETRONAS |
publishDate |
2014 |
url |
http://utpedia.utp.edu.my/18292/1/Final%20report.pdf http://utpedia.utp.edu.my/18292/ |
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1739832486682165248 |
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13.160551 |