globalchange  > 过去全球变化的重建
DOI: 10.1306/01191110090
Scopus记录号: 2-s2.0-80053397293
论文题名:
Petroleum systems of the Simeulue fore-arc basin, offshore Sumatra, Indonesia
作者: Lute R.; Gaedicke C.; Berglar K.; Schloemer S.; Franke D.; Djajadihardja Y.S.
刊名: AAPG Bulletin
ISSN: 0149-1834
EISSN: 1558-9564
出版年: 2011
发表日期: 2011
卷: 95, 期:9
起始页码: 1589
结束页码: 1616
语种: 英语
Scopus关键词: Amplitude versus offset ; Back-arc ; Bottom simulating reflector ; Bright spots ; Carbonate build-up ; Deep burials ; Depocenters ; Fore-arc basin ; Geochemical prospecting ; Geophysical data ; Heat-flow ; Hydrocarbon generation ; Hydrocarbon potential ; Hydrocarbon reservoir ; Miocene ; Multichannel seismic data ; Oil and gas ; Petroleum systems ; Plate convergence ; Source rocks ; Sumatra ; Sumatra , Indonesia ; Surface sample ; Analytical geochemistry ; Heat transfer ; Hydrocarbons ; Offshore oil wells ; Petroleum geology ; Petroleum prospecting ; Petroleum reservoir evaluation ; Seismology ; Wells ; Three dimensional ; forearc basin ; geophysical method ; heat flow ; hydrocarbon generation ; hydrocarbon reservoir ; petroleum hydrocarbon ; plate convergence ; reservoir characterization ; seismic data ; source rock ; Aceh ; Greater Sunda Islands ; Indonesia ; Simeulue ; Sumatra ; Sunda Isles ; Calluna vulgaris
Scopus学科分类: Energy ; Earth and Planetary Sciences
英文摘要: Forearc basins result from plate convergence. These basins are situated offshore between an outer-arc high and the mainland. Historically, these regions have not been considered important petroleum provinces partly because low heat flow may limit significant thermal hydrocarbon generation. The Simeulue forearc basin extends between Simeulue Island and northern Sumatra. It is a frontier shallow shelf area with few wells and no wells in the basin center; therefore, it is studied using geophysical data and geologic surface samples. Multichannel seismic data show bright spots above potential hydrocarbon reservoirs in carbonate buildups. Amplitude versus offset analyses indicate the presence of gas, and surface geochemical prospecting suggests thermal hydrocarbon generation. Heat flow in the Simeulue Basin ranges between 37 and 74 mW/m 2, as deduced from one-dimensional petroleum system modeling and bottom-simulating reflector depths. Two possible source rocks (Eocene and lower-middle Miocene) were assigned for three-dimensional petroleum system modeling in the Simeulue Basin. Because of a similar pre-Miocene geologic evolution of the present-day back arc and the fore arc, it can be assumed that the back-arc source rocks also occur in the fore arc. Modeling based on two heat-flow scenarios (40 and 60 mW/m2) reveals that oil and gas generation is possible within and below the main depocenters of the central and southern Simeulue Basin. This study shows that deep burial (<6 km [<3.7 mi]) of source rocks can compensate for low heat flow. Therefore, forearc basins may be more prolific for hydrocarbons than previously considered, and each forearc basin should be studied carefully to evaluate its hydrocarbon potential. © 2011. The American Association of Petroleum Geologists.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-80053397293&doi=10.1306%2f01191110090&partnerID=40&md5=55389ed0e3efab395994cb2d517abf0c
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/13403
Appears in Collections:过去全球变化的重建
影响、适应和脆弱性
科学计划与规划
气候变化与战略
全球变化的国际研究计划
气候减缓与适应
气候变化事实与影响

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Recommended Citation:
Lute R.,Gaedicke C.,Berglar K.,et al. Petroleum systems of the Simeulue fore-arc basin, offshore Sumatra, Indonesia[J]. AAPG Bulletin,2011-01-01,95(9)
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