76 Trapping Mechanisms along North Similan and Lanta Trends, Pattani Basin, Gulf of Thailand Bulletin of Earth Sciences of Thailand
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Program in Petroleum Geoscience, Faculty of Science, Chulalongkorn University, Bangkok, Thailand 2Basin Analysis and Structural Evolution BASE Research Unit, Department of Geology,
Map illustrating the distributions of the calculated b values for the 13 seismic source zones zone A–M proposed in the mainland Southeast Asia MSEA , scaling from Pailoplee and Choowong
In seismic section, Triassic sediments show termination rotated onlap on high amplitude peak of irregular top Zechstein horizon, this indicate that top Zechstein reflector should be
The use of linear scales in spectral decomposition proves a better method for distinguishing between two equally thin layers in a vertical view, whereas the use of octave scale can be
The seismic cross section along drilled wells and logging interpretation were used to calibrate horizons stack and separate into minor horizon, total fifty-two-layers horizons with
3.2 Middle Miocene Non-marine coaly mudstone-6, marginal marine coaly mudstone-1, and estuarine shale 2 have been selected to represent the likely distribution of organic-rich facies
Figure 13 The left block stratigraphy C- This unit of deposition fines upwards from a clast supported cobble conglomerate to interbedded sands and gravels in massive mudstone.. The
