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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محفوظ في:
التفاصيل البيبلوغرافية
المؤلف الرئيسي: FAUZI, Achmad
التنسيق: Theses and Dissertations NonPeerReviewed
منشور في: [Yogyakarta] : Universitas Gadjah Mada 2013
الموضوعات:
الوصول للمادة أونلاين: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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spelling id-ugm-repo.1236512016-04-14T02:34:19Z https://repository.ugm.ac.id/123651/ Stratigrafi Seismik untuk Interpretasi Fasies Pengendapan Berdasarkan Data Seismik 2D pada Daerah Lepas Pantai Onin, Palung Seram FAUZI, Achmad Stratigraphy (incl. Biostratigraphy and Sequence Stratigraphy) 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 [Yogyakarta] : Universitas Gadjah Mada 2013 Thesis NonPeerReviewed FAUZI, Achmad (2013) Stratigrafi Seismik untuk Interpretasi Fasies Pengendapan Berdasarkan Data Seismik 2D pada Daerah Lepas Pantai Onin, Palung Seram. Bachelor thesis, Universitas Gadjah Mada. http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=63765
institution Universitas Gadjah Mada
building UGM Library
country Indonesia
collection Repository Civitas UGM
topic Stratigraphy (incl. Biostratigraphy and Sequence Stratigraphy)
spellingShingle Stratigraphy (incl. Biostratigraphy and Sequence Stratigraphy)
FAUZI, Achmad
Stratigrafi Seismik untuk Interpretasi Fasies Pengendapan Berdasarkan Data Seismik 2D pada Daerah Lepas Pantai Onin, Palung Seram
description 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
format Theses and Dissertations
NonPeerReviewed
author FAUZI, Achmad
author_facet FAUZI, Achmad
author_sort FAUZI, Achmad
title Stratigrafi Seismik untuk Interpretasi Fasies Pengendapan Berdasarkan Data Seismik 2D pada Daerah Lepas Pantai Onin, Palung Seram
title_short Stratigrafi Seismik untuk Interpretasi Fasies Pengendapan Berdasarkan Data Seismik 2D pada Daerah Lepas Pantai Onin, Palung Seram
title_full Stratigrafi Seismik untuk Interpretasi Fasies Pengendapan Berdasarkan Data Seismik 2D pada Daerah Lepas Pantai Onin, Palung Seram
title_fullStr Stratigrafi Seismik untuk Interpretasi Fasies Pengendapan Berdasarkan Data Seismik 2D pada Daerah Lepas Pantai Onin, Palung Seram
title_full_unstemmed Stratigrafi Seismik untuk Interpretasi Fasies Pengendapan Berdasarkan Data Seismik 2D pada Daerah Lepas Pantai Onin, Palung Seram
title_sort stratigrafi seismik untuk interpretasi fasies pengendapan berdasarkan data seismik 2d pada daerah lepas pantai onin, palung seram
publisher [Yogyakarta] : Universitas Gadjah Mada
publishDate 2013
url 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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