川西温江构造浅中层勘探潜力分析
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摘要
构造演化分析认为,温江构造为古今叠合型构造,紧邻上三叠统生气中心。西侧发育作为油气运移通道的彭县断层,有利于天然气运聚成藏。化探和钻井揭示,深层的天然气已经运移到浅层,并聚集成藏。蓬莱镇组、遂宁组为三角洲平原亚相沉积,蓬莱镇组的“低频、强振幅”地震异常比较发育,反映储集砂体发育。用容积法计算,浅中层圈闭资源量达401×108m3,表明温江构造浅中层是近期勘探的有利目标。
Tectonic evolution analysis indicates that Wenjiang Structure is a palaeo-present-congruent structure and very close to Upper Triassic gas-generating center. As a petroleum migration channel, the Pengxian Fault, developed at west of the structure, is favorable for gas accumulation and forming a reservoir. Geochemical exploration and drilling show that deep gas has migrated into shallow formations to accumulate and form the reservoir. Penglaizhen and Suining formations deposit at deltaic-plain facies. For the former, abnormal seismic is almost characterized by low frequency and strong amplitude, reflecting a well-developed sandbody. The resource of shallow and middle traps reaches to 401×10~8m~3 by the volume method, which suggests the shallow- and middle-formations in Wenjiang Structure are favorable prospects for recent exploration.
引文
1曾允孚,夏文杰·沉积岩石学〔M〕·北京:地质出版社,1986
    2李书兵,叶军·川西坳陷致密碎屑岩天然气成藏主控因素及大中型气田勘探新目标研究·中石化西南石油局地质综合研究院科研成果,2000
    3李书兵·川西坳陷远源气藏成藏主控因素分析·川西坳陷致密碎屑岩领域天然气成藏理论及勘探开发方法技术·北京:地质出版社,2003
    4邓康龄·成都平原侏罗系气藏形成机理·天然气工业,1999,19(增刊)

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