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作 者:Gaokui Wu Fanjun Kong Naxin Tian Tianbi Ma Chongzhi Tao
机构地区:[1]Petroleum Exploration and Production Research Institute,SINOPEC,Beijing,102206,China
出 处:《Energy Geoscience》2023年第3期71-79,共9页能源地球科学(英文)
基 金:supported by the National Science and Technology Major Project of China(2016ZX05033);the Project of SINOPEC Science and Technology Department(P19021-2);the Basic Prospective Research Project of SINOPEC(P22214-2).
摘 要:Commercial hydrocarbon reservoirs have been discovered in shallow-water areas of the Scotian Basin, Eastern Canada. However, knowledge about the structure and hydrocarbon accumulation characteristics of the basin is still insufficient, which constrains the oil and gas exploration in deep-water areas. Based on comprehensive data of magnetic anomalies, seismic survey, and drilling, this study determines the structure characteristics of the Scotian Basin and its hydrocarbon accumulation conditions in deep waters and evaluates the deep-water hydrocarbon exploration potential. The transform faults and basement structures in the northern basin control the sedimentary framework showing thick strata in east and thin strata in west of the basin. The bowl-shaped depression formed by thermal subsidence during the transitional phase and the confined environment (micro basins) caused by salt tectonics provide favorable conditions for the development of source rocks during the depression stage (also referred to as the depression period sequence) of the basin. The progradation of large shelf-margin deltas during the drift phase and steep continental slope provide favorable conditions for the deposition of slope-floor fans on continental margins of the basin. Moreover, the source-reservoir assemblage comprising the source rocks within the depression stage and the turbidite sandstones on the continental margin in the deep waters may form large deep-water turbidite sandstone reservoirs. This study will provide a valuable reference for the deep-water hydrocarbon exploration in the Scotian Basin.
关 键 词:Transform fault Salt tectonic Hydrocarbon accumulation model Deep-water turbidite sandstone Scotian basin
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