Bulletin of Earth Sciences of Thailand
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Dokumen terkait
XRD and SEM indicate rock quality in the sandstone reservoirs was influenced by a variety of authigenic minerals, such as carbonate cements, quartz overgrowths, zeolites, and
Minor structural trend of breccia and major NNW trend of massive conform NNW strike-slip fault in The minor trend of dyke in NE-SW direction probably controls by NE striking fault in
Unit Kh-4 The unit Kh-4 is interpreted as tidal sand flat which is 36 m in thickness and comprises of thick bedded coarsening upward fine to medium grain sandstone.. Basal fine grain
4.2 Reservoir evaluation and prospectivity The analysis of seismic interpretation data, paleogeographic maps, well data and biostratigraphy information suggests that the possible
3.2 Stratigraphic architecture and depositional environments Stratigraphic architecture Based on facies and facies association, four architectural elements were identified in
From plotting, the major oxide of samples from this study and previous studies of Wang Pong volcanic rocks and Wichian Buri volcanic rocks Figure 5B., we found that G2 and G4
Thus, strike-slip faults are not responsible for opening all rift basins in Thailand; subduction rollback of the Indian plate to the west of Thailand is possibly an alternative
Structural geology related with fracture development and fluid evolution at Khao Tham Phedan, Nakhon Sawan Province, Central Thailand Thanaset Chuchaem* Petroleum Geoscience
