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IDENTIFICATION OF POTENTIAL SOURCE ROCKS USING SEISMIC ATTRIBUTES IN THE SYN-RIFT STRATIGRAPHIC SEQUENCE IN THE SOUTHERN PATTANI BASIN, GULF OF THAILAND |
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| รหัสดีโอไอ | |
| Creator | Chanmaly Chhun |
| Title | IDENTIFICATION OF POTENTIAL SOURCE ROCKS USING SEISMIC ATTRIBUTES IN THE SYN-RIFT STRATIGRAPHIC SEQUENCE IN THE SOUTHERN PATTANI BASIN, GULF OF THAILAND |
| Contributor | - |
| Publisher | Department of Geology, Chulalongkorn University |
| Publication Year | 2558 |
| Journal Title | Bulletin of Earth Sciences of Thailand (BEST) |
| Journal Vol. | 7 |
| Journal No. | 2-Jan |
| Page no. | 230-239 |
| Keyword | Oligocene stratigraphy, organic-rich shale, high radiogenic shale, amplitude |
| URL Website | https://www.bestjournal.org/ |
| Website title | Bulletin of Earth Sciences of Thailand |
| ISSN | 1906-280X |
| Abstract | Estimation of source rock distribution is required to determine hydrocarbon charge in the reservoir. In the Gulf of Thailand, the southern Pattani Basin has limited wells that penetrate into the source rock and the size of the source rock volume is also unknown. Thus seismic facies mapping is the only way to map source rock distribution in the undrilled areas of the Basin. Mancharee_1 and Mayura_1 exploration wells drilled into Oligocene stratigraphy. Based on log analysis in the Oligocene interval, these two wells encountered organic-rich shale and a high radiogenic shale zone considered as the potential source rock due to their low AI (Acoustic Impedance) and high GR (Gamma Ray) values. This is the main characteristics of source rocks as they generally have decreasing AI due to increasing organic contents which reduces its density, velocity, and has a high GR. Based on AI difference, there will be contrasting reflections of source rock shale, sandstone, and shale in the study area. Matching well logs to seismic for seismic facies recognition of source rock showed that the top of source rock (top Oligocene) is represented as a trough. These potential source rocks give negative and positive reflection amplitudes. Consequently, the study of source rock distribution and mapping on seismic in areas of the Basin with no well penetrations including deeper parts of the Basin is very important for prediction of hydrocarbon generation. In deeper parts of the Basin, source rock formation would be expected to occur and have a possible high TOC content and maturity. This results in a decreasing AI in source rock compared to other rock types; hence the reflection amplitudes of source rock shales give strong negative and positive amplitudes. By using seismic data, the source rock delineation and thickness therefore can be mapped. The result of mapping source rock distribution is indispensable for petroleum system prediction. |
