Sedimentology and Origin of Microporosity in Miocene Carbonate Platforms, Central Luconia, offshore Sarawak, Malaysia
Central Luconia is situated in the north of Bintulu in a water depth of approximately 40-160 feet. In the mid-sixties, a large number of Miocene carbonate buildups were seismically detected in the offshore shelf area of the Central Luconia province. Especially in the north, a chain of deeply buried...
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oai:utpedia.utp.edu.my:189712023-05-15T07:41:11Z http://utpedia.utp.edu.my/id/eprint/18971/ Sedimentology and Origin of Microporosity in Miocene Carbonate Platforms, Central Luconia, offshore Sarawak, Malaysia JANJUHAH, HAMMAD TARIQ QE Geology Central Luconia is situated in the north of Bintulu in a water depth of approximately 40-160 feet. In the mid-sixties, a large number of Miocene carbonate buildups were seismically detected in the offshore shelf area of the Central Luconia province. Especially in the north, a chain of deeply buried carbonate buildups are present, located west of the Baram hinge line. These buildups were generally covered by 3000-6000 ft of clastics, whereby a higher burial depth was observed for buildups located in the north of Central Luconia. Drilling activity started in 1967 and some 60 buildups were tested. The resulting discovery of six giant gas fields and some 20 smaller accumulations make this area an important gas province. 2018-04 Thesis NonPeerReviewed application/pdf en http://utpedia.utp.edu.my/id/eprint/18971/1/final%20list%20of%20contents.pdf application/pdf en http://utpedia.utp.edu.my/id/eprint/18971/2/Full%20Thesis%20after%20Viva%20%28Corrected%29%20April%202018%20-%20Copy.pdf JANJUHAH, HAMMAD TARIQ (2018) Sedimentology and Origin of Microporosity in Miocene Carbonate Platforms, Central Luconia, offshore Sarawak, Malaysia. PhD. thesis, Universiti Teknologi PETRONAS. |
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QE Geology JANJUHAH, HAMMAD TARIQ Sedimentology and Origin of Microporosity in Miocene Carbonate Platforms, Central Luconia, offshore Sarawak, Malaysia |
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Central Luconia is situated in the north of Bintulu in a water depth of approximately 40-160 feet. In the mid-sixties, a large number of Miocene carbonate buildups were seismically detected in the offshore shelf area of the Central Luconia province. Especially in the north, a chain of deeply buried carbonate buildups are present, located west of the Baram hinge line. These buildups were generally covered by 3000-6000 ft of clastics, whereby a higher burial depth was observed for buildups located in the north of Central Luconia. Drilling activity started in 1967 and some 60 buildups were tested. The resulting discovery of six giant gas fields and some 20 smaller accumulations make this area an important gas province. |
format |
Thesis |
author |
JANJUHAH, HAMMAD TARIQ |
author_facet |
JANJUHAH, HAMMAD TARIQ |
author_sort |
JANJUHAH, HAMMAD TARIQ |
title |
Sedimentology and Origin of Microporosity in Miocene Carbonate Platforms, Central Luconia, offshore Sarawak, Malaysia |
title_short |
Sedimentology and Origin of Microporosity in Miocene Carbonate Platforms, Central Luconia, offshore Sarawak, Malaysia |
title_full |
Sedimentology and Origin of Microporosity in Miocene Carbonate Platforms, Central Luconia, offshore Sarawak, Malaysia |
title_fullStr |
Sedimentology and Origin of Microporosity in Miocene Carbonate Platforms, Central Luconia, offshore Sarawak, Malaysia |
title_full_unstemmed |
Sedimentology and Origin of Microporosity in Miocene Carbonate Platforms, Central Luconia, offshore Sarawak, Malaysia |
title_sort |
sedimentology and origin of microporosity in miocene carbonate platforms, central luconia, offshore sarawak, malaysia |
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2018 |
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http://utpedia.utp.edu.my/id/eprint/18971/1/final%20list%20of%20contents.pdf http://utpedia.utp.edu.my/id/eprint/18971/2/Full%20Thesis%20after%20Viva%20%28Corrected%29%20April%202018%20-%20Copy.pdf http://utpedia.utp.edu.my/id/eprint/18971/ |
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