Stratigrafi Seismik untuk Interpretasi Fasies Pengendapan Berdasarkan Data Seismik 2D pada Daerah Lepas Pantai Onin, Palung Seram
geology especially Onin offshore areas, Seram Trough is one of the target areas of hydrocarbon exploration in eastern Indonesia are generally only available seismic data. The seismic data can assist in the assessment of subsurface stratigraphic through the seismic stratigraphic approach. eismic...
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格式: | Theses and Dissertations NonPeerReviewed |
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[Yogyakarta] : Universitas Gadjah Mada
2013
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在線閱讀: | https://repository.ugm.ac.id/123651/ http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=63765 |
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機構: | Universitas Gadjah Mada |
總結: | geology especially
Onin offshore areas, Seram Trough is one of the target areas of
hydrocarbon exploration in eastern Indonesia are generally only available seismic
data. The seismic data can assist in the assessment of
subsurface stratigraphic through the seismic stratigraphic approach.
eismic S stratigraphic is interpretation of stratigraphy from seismic data
(Vail & Mitchum, 1997 in Sukmono, 1999) in which there is discussion of
seismic sequence and depositional facies.
etermination of s D eismic sequence and depositional facies are the result of
this study which are useful for studying hydrocarbon prospects. Sequences which
can be identifiable are nine. Sequence one is equivalent with Bogal Limestone
which is dominated by shelf/platform facies, sequence two is equivalent with
Yefbie Shale which is dominated by delta plain facies, sequence three is
equivalent with Demu Formation and Lelinta Shale which is dominated by delta
front, sequence four is interpretated with Facet Group which is dominated by
proximal basin and lower slope facies, sequence five is equivalent with Lower
New Guinea Limestone which is dominated by shelf/platform facies, sequence
six is equivalent with Upper New Guinea Limestone which is dominated by
shelf/platform facies, sequence seven is equivalent transgression sequence which
developed submarine canyon fill facies, sequence eight is equivalent
progradasional sequence 1 which developed slope facies, sequence nine is
equivalent progradasional sequence 2 which developed marine (slope) onlap.
facies |
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