STRATIGRAPHY, PALEONTOLOGY, GEOCHEMISTRY, PALEOGEOGRAPHY AND HYDROCARBON POTENTIAL OF THE UPPER PALEOZOIC KINTA LIMESTONE. PENINSULAR MALAYSIA
The Southeast Asia terranes derived from the Gondwana margms m the Carboniferous-Triassic time have a complex basin evolution in the Paleo-Tethys. Based on major stratigraphic. geological, geophysical and tectonic phenomena, the Peninsular Malaysia is divided into Western, Central, and Eastern te...
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Format: | Thesis |
Language: | English |
Published: |
2016
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Online Access: | http://utpedia.utp.edu.my/21926/1/2016%20-PETROLEUM%20GEOSCIENCES%20-%20STRATIGRAPHY%2C%20PALEONTOLOGY%2C%20GEOCHEMISTRY%2C%20PALEOGEOGRAPHY%20AND%20HYDROCARBON%20POTENTIAL%20OF%20THE%20UPPER%20PALEOZOIC%20KINTA%20LIMESTONE%2C%20PENINSULAR.pdf http://utpedia.utp.edu.my/21926/ |
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Institution: | Universiti Teknologi Petronas |
Language: | English |
Summary: | The Southeast Asia terranes derived from the Gondwana margms m the
Carboniferous-Triassic time have a complex basin evolution in the Paleo-Tethys.
Based on major stratigraphic. geological, geophysical and tectonic phenomena, the
Peninsular Malaysia is divided into Western, Central, and Eastern tectonostratigraphic
belts. Within the Western Belt, the Kinta Limestone is a voluminous
succession, representing 65% of the Paleozoic in the Kinta Valley. Owing to
structural and tectono-thermal complexities; sedimentological and paleontological
works in these carbonates have proven to be problematic. |
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