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APPLICATION OF POST-STACK SEISMIC INVERSION AND ITS LIMITATIONS FOR MAPPING OF FLUVIAL SYSTEMS IN WESTERN PATTANI BASIN, GULF OF THAILAND Phanat Thatmali |
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| รหัสดีโอไอ | |
| Creator | Phanat Thatmali |
| Title | APPLICATION OF POST-STACK SEISMIC INVERSION AND ITS LIMITATIONS FOR MAPPING OF FLUVIAL SYSTEMS IN WESTERN PATTANI BASIN, GULF OF THAILAND Phanat Thatmali |
| Contributor | - |
| Publisher | Department of Geology, Chulalongkorn University |
| Publication Year | 2559 |
| Journal Title | Bulletin of Earth Sciences of Thailand (BEST) |
| Journal Vol. | 8 |
| Journal No. | 2 |
| Page no. | 94-102 |
| Keyword | P-impedance, post-stack seismic inversion, marginal marine coaly mudstone, Pattani basin |
| URL Website | https://www.bestjournal.org/ |
| Website title | Bulletin of Earth Sciences of Thailand |
| ISSN | 1906-280X |
| Abstract | Reservoir rocks in the Pattani Basin are fluvial sandstones which are highly compartmentalized due to their complex depositional and structural evolution. Imaging of these reservoirs is not always possible using conventional seismic data. This study presents rock physics analysis for the feasibility of post-stack seismic inversion within different sequences of the western part of the Pattani Basin. The post-stack seismic inversion was executed for the mapping of fluvial reservoir sands. Rock-physics results reveal that P-impedance values of sands are less than shales in the late Middle Miocene and Early Miocene depositional sequences. Some of the thin shales within the early Middle Miocene have very low P-impedance that is equivalent to sands. These are interpreted as marginal marine coaly mudstones. Blind tests demonstrated that sands could be differentiated from shales in Early Miocene and partially differentiated in the late Middle Miocene sequences. Geomorphological analysis of horizon slices extracted from P-impedance volumes showed that sands associated with the channels are narrow and of high sinuosity in the Early Miocene and early Middle Miocene, whereas wide channels were observed in the late Middle Miocene. Marine influence has been inferred from the presence of marginal marine coaly mudstone. The marine incursions are more dominant in early Middle Miocene sequence and initiated in Early Miocene from the southeastern part of the area. |
