Depositional Environment of Sands Beneath the Mid-Miocene Unconformity in the Plamuk-L and Surat-C Field Areas, Gulf of Thailand, Using Cuttings Identification, Well Log and Seismic Interpretation
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Creator Phansom Suksirisamphan
Title Depositional Environment of Sands Beneath the Mid-Miocene Unconformity in the Plamuk-L and Surat-C Field Areas, Gulf of Thailand, Using Cuttings Identification, Well Log and Seismic Interpretation
Contributor -
Publisher Department of Geology, Chulalongkorn University
Publication Year 2553
Journal Title Bulletin of Earth Sciences of Thailand (BEST)
Journal Vol. 3
Journal No. 2
Page no. 49-51
Keyword MMU, Plamuk-L, Surat-C, Red Bed, sand, channel point-bars
URL Website https://www.bestjournal.org/
Website title Bulletin of Earth Sciences of Thailand
ISSN 1906-280X
Abstract The sub-MMU sand in the Plamuk-L and Surat-C areas is a blocky, extensive thick sand (40-60 ft thick), deposited below the MMU and within the Upper Red Bed unit (Sequence IV), which was deposited under more oxic-conditions during exposure in a marine regression. This sand shows 23% - 34% porosity and 8% - 11% clay volume, which qualifies it as a good quality potential reservoir. Regional sand features interpreted from seismic amplitude map show pocket-like shapes, aligned along a tortuous trend in a northeast southwest direction. This distribution indicates variations that are likely tied to deposition as channel point-bars. The studied sand is filled with oil and gas in wells drilled into closed structures (SUWC-32 and 33), while hydrocarbons are absent in areas of non-closure.
Chulalongkorn University

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