Sukmono, S., 1999, Interpretasi Seismik Refleksi, Jurusan Teknik Geofisika, Institut Tektologi Bandung, tidak diterbitkan. The Role Of Strike Slip Faulting In Structural Development Of The North Sumatra Basin, 14th Annual Convention, IPA Proceeding, Jakarta. et al, 1989, Sedimentary Environment from Wireline Logs : Schlumberger. Davies., 1984, Tertiary Structural Evolution And Related Hydrocarbon Occurrences, North Sumatra Basin, 13th Annual Convention, IPA Proceeding, Jakarta. North sumatra,7th annual convention, IPA Proceeding, Jakarta. Mulhadiono, et al., 1978, The middle Baong sandstone unit as one of the most prospective units In the Aru area. Mulhadiono, 1976, Depositional study of Lower Keutapang in the Aru Area, North Sumatra, 5th Annual Convention, IPA Proceeding, Jakarta. Payton, Seismic Stratigraphy – Application to Hydrocarbon Exploration : AAPG Memoir 26, p. Mitchum, R.M., 1997, Seismic Stratigraphy and Global Changes of Sea Level, dalam C.E. Koesoemadinata, R.P., 1971, Teknik Evaluasi Geologi Bawah Permukaan,ITB, Bandung, Indonesia. Koesoemadinata, R.P., 1980, Geologi Minyak dan Gas Bumi, jilid I dan II, ITB, Bandung. Koesoemadinata R.P., 2001, Petroleum Potential of Indonesia : Geology of Petroleum Basins of Indonesia, Prosiding Ikatan Ahli Geologi Indonesia, Pertemuan Ilmiah Tahunan XXX, Yogyakarta
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Karig, D.E, 1980, Structural framework of the fore-arc basin, NW Sumatera, Journal Geologi Soc. Harsono, A., 1997, Evaluasi Formasi dan Aplikasi Log : Sclumberger Oil Field, Edisi ke 8, Jakarta. Ğubank & Makki, 1981, Structural Geology of Central Sumatra Back Arc Basin : Proceed 10th Ann. (2000), An Outline of The Geology of Indonesia, IAGI 2000
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The Geological Evolution Of Northern Sumatra, 9th Annual Convention, IPA Proceeding, Jakarta. Studi Pengelolaan Cadangan dan Sumber Daya Hidrokarbon, buku-2, Unpublised report Clastic origin of this deposits were interpreted came from South-South West direction or from Bukit Barisan where at that time is started to uplift. In this episode, there is a change in depositional setting from bathyal to middle neritic. while Middle Baong Sand are deposited in the minor falling stage placed at N13 (Middle of Middle Miocene). Baong Formation are deposited when the sea level are rising regionally at Middle Miocene (N7-N15) makes the sediment deposited in deep water environment. Based on the analyses in 39 seismic sections and 2 wireline log, the area are consist of three depositional sequences, namely sequence I (consist of HST I) Sequence II (consist of TST II and LST II), and Sequence III (consist of TST III). The study can be used in ranking the prospect for new oil field.
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The analyses aim to understand the sedimentation pattern regarding to sequence stratigraphy model including its lateral and vertical succession based on seismic and well data. This paper defines the stratigraphic sequence focused on Middle Baong Sand.