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Seismic Facies Interpretation of Fluvial/Marginal Marine Sand Architecture in Kra Basin, Gulf of Thailand |
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| รหัสดีโอไอ | |
| Creator | Parichat Wainuson |
| Title | Seismic Facies Interpretation of Fluvial/Marginal Marine Sand Architecture in Kra Basin, Gulf of Thailand |
| Contributor | - |
| Publisher | Department of Geology, Chulalongkorn University |
| Publication Year | 2555 |
| Journal Title | Bulletin of Earth Sciences of Thailand (BEST) |
| Journal Vol. | 5 |
| Journal No. | 2 |
| Page no. | 86-94 |
| Keyword | Kra Basin, Fluvial Sand Architecture, Stratal Slices |
| URL Website | https://www.bestjournal.org/ |
| Website title | Bulletin of Earth Sciences of Thailand |
| ISSN | 1906-280X |
| Abstract | The study area lies in the Kra basin, Gulf of Thailand covering an area of approximately 990 sq.kms. The goal of this study is to understand the distribution and architecture of fluvial sand systems by analyzing the seismic facies based on 3D seismic images in the interval of interest from the Middle Miocene to Recent. Three wells are located in this area but only one has a good well to seismic tie. The seismic facies interpretation used the stratal slicing method based on several key horizons which is able to handle the nonflat lying deeper formations and time slices in the very shallow section. The seismic images from stratal slices and time slices illustrate the complex fluvial systems for the whole interval with minor marine influence in the shallow section. Nine distinct fluvial styles were interpreted which are single small channels, small to medium channel meander belts, tidal creeks, incised valley fills, high-sinuosity channels with large point bars, moderate to high-sinuosity channels with moderate point bars, high-sinuosity small channels with narrow point bars, low to moderate-sinuosity small channels with narrow point bars, and low-sinuosity large channels with no point bar. The results show that the variety of fluvial styles deposit sand within point bars with a dramatic range of sand body dimensions. The fluvial styles are dominantly influenced by variations in discharge rate, sediment load, climate and basin topography. Relative sea-level changes have an effect mainly in the shallow section. In term of reservoir implication, the high-sinuosity channels with large point bars associated with large channels give the greatest volume of porous reservoir facies whereas small channels deposit thin sands with limited areal extent and volume. |
