Please use this identifier to cite or link to this item: http://hdl.handle.net/123456789/362
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dc.contributor.authorSulaiman, N.en_US
dc.contributor.authorAbd. Samad, M.A.S.en_US
dc.contributor.authorSulaiman, N.en_US
dc.contributor.authorAli Khan, M.M.en_US
dc.contributor.authorRosmadi, N.S.en_US
dc.date.accessioned2021-01-17T04:20:05Z-
dc.date.available2021-01-17T04:20:05Z-
dc.date.issued2020-09-
dc.identifier.issn17551307-
dc.identifier.urihttp://hdl.handle.net/123456789/362-
dc.descriptionScopusen_US
dc.description.abstractThis study aims to interpret the seismic facies and geological structures of the Miocene-Pleistocene succession based on the 3-D seismic dataset. The seismic data was interpreted by using Kingdom 8.8 version software. The dimension of study area is approximately 187 km2 (14.8 km long by 12.6 km wide). The variable types of seismic facies and geological structures were determined from the horizontal (inline) and vertical (crossline) lines in 2D seismic section of study area. The seismic facies can be classified into for major seismic facies such as parallel and sub-parallel, wavy, facies that reach out to south-east and chaotic reflector. Parallel and semi-parallel facies consist from high amplitude to low amplitude and moderate to high continuity. The mounded discontinuous seismic facies also can be seen in the seismic section and can be interpreted as turbidities depositional environment at the two-way time (TWT) ranges from 1.4 to 1.5 ms. The chaotic facies contain natural gas as it display due to an error to a wave at the two-way time ranges from 1.0 to 1.1 ms. The geological structures were determined at the study area consists of anticlines, syncline and faults that can be interpreted as structural and stratigraphic trap for potential hydrocarbon.en_US
dc.language.isoenen_US
dc.publisherIOP Publishing Ltden_US
dc.relation.ispartofIOP Conference Series: Earth and Environmental Scienceen_US
dc.subjectDepositionen_US
dc.subjectStratigraphyen_US
dc.subjectDepositional environmenten_US
dc.subjectGeological structuresen_US
dc.subjectsHigh amplitudesen_US
dc.titleSeismic Facies and Geological Structure Interpretation of the A-Field, Malay Basin, Malaysiaen_US
dc.typeInternationalen_US
dc.relation.conference2nd International Conference on Tropical Resources and Sustainable Sciences, CTReSS 2020en_US
dc.identifier.doi10.1088/1755-1315/549/1/012019-
dc.volume549 (1)en_US
dc.description.articleno012019en_US
dc.date.seminarstartdate2020-08-10-
dc.date.seminarenddate2020-08-11-
dc.description.placeofseminarUniversiti Malaysia Kelantan, City Campus Kelantan; Malaysiaen_US
dc.description.typeProceeding Papersen_US
item.grantfulltextopen-
item.languageiso639-1en-
item.openairetypeInternational-
item.fulltextWith Fulltext-
crisitem.author.deptUNIVERSITI MALAYSIA KELANTAN-
crisitem.author.deptUniversiti Malaysia Kelantan-
crisitem.author.deptUniversity Malaysia Kelantan, Malaysia-
crisitem.author.orcid0000-0001-9737-3177-
Appears in Collections:Faculty of Earth Science - Proceedings
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