中国西部叠合盆地油气藏形成、演化与分布预测
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国家重点基础研究发展计划(973计划)


Hydrocarbon reservoirs formation, evolution and distribution in the superimposed basin, Western China
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    摘要:

    中国西部叠合盆地经历了多期构造变动和多旋回的油气成藏作用,研究叠合盆地油气藏的形成、演化和分布预测具有重要的意义。叠合盆地指不同时期形成的不同类型的沉积盆地或地层在同一地理位置上的叠加和复合,具有地层沉积不连续、地层构造不连续、地层应力应变作用不连续等三大标志性特征,依据构造剖面上地层年代的关联性,将叠合盆地分为五种类型,即连续沉积型叠合盆地、中晚期地层叠合盆地、早晚期地层叠合盆地、早中期地层叠合盆地、长期暴露型叠合盆地。叠合盆地普遍发育复杂油气藏,三种作用(剥蚀作用、断裂作用、褶皱作用)六种机制(渗漏、扩散、溢散、氧化、降解和裂解)形成复杂油气藏,依据成因特征分为五类,原成型油气藏,圈闭调整型油气藏,组分变异型油气藏,相态转换型油气藏,规模改造型油气藏。研究表明,复杂油气藏中天然气的地下产状特征和分布特征与地表产状特征和分布特征有很大差异。中国西部叠合盆地油气分布主要受烃源灶、古隆起、沉积相、断裂带、构造变动和区域盖层等六大因素的控制。其中烃源灶(S)、古隆起(M)、沉积相(D)和盖层(C)等四大要素控制着油气成藏的形成和分布,并建立了多要素匹配(T-CDMS)成藏模式,用以预测有利成藏领域。油气藏形成之后,多期的构造变动对早成的油气藏进行调整、改造和破坏,主要受构造变动强度、构造变动时间、构造变动次数、构造变动时盖层的封油气性能等四大要素控制,并以此建立了多期构造变动破坏油气藏后剩余潜力评价模型,利用这一模型可以预测出有利勘探区带并评价出有利勘探区带中的剩余资源潜力。油气藏经过改造,表现出晚期成藏效应,并受相势耦合作用的控制最后定位,利用晚期成藏效应和相势耦合理论可以预测有利勘探目标,并指出潜在有利勘探目标。

    Abstract:

    There are multi-stages tectonic events and hydrocarbon accumulation happened in the superimposed basin, Western China, it is great of significant to study the hydrocarbon reservoirs formation, evolution and distribution in the superimposed basin. Superimposed Basin means the different types sedimentary basin or strata superimpose and overlap in the same geographic location at different stages, which has the three marked characteristics of discontinuous of sedimentary, structure and stress-strain. It can be divided into the following five types according to the chronologicage relation of structural section: successive sedimentation superimposed basin, strata superimposed at middle and late stage superimposed basin, strata superimposed at early and late stage superimposed basin, strata superimposed at early and late stage superimposed basin, and long term exposure superimposed basin. The complicated hydrocarbon reservoirs general developed which formed by three effects (erosion, faulting and folding) and six mechanisms (leakage, diffusion, spilling, oxidation, degradation and fragmentation). It can be divided into the following five types according to the genesis: Original hydrocarbon reservoirs, trap adjustment hydrocarbon reservoirs, component variant hydrocarbon reservoirs, phase transition hydrocarbon reservoirs and scale transformation hydrocarbon reservoirs. The study results show that the gas occurrence characteristics and distribution in the complex hydrocarbon reservoirs are very different between underground and surface. The hydrocarbon distribution is mainly affected by source kitchen, paleo-mountain, deposit facies, faults, tectonic events and regional caprocks, among them, the four major elements, source rock (S), Paleo-mountain (M), deposit facies (D) and regional caprocks (C) control the hydrocarbon accumulation and distribution, and build the hydrocarbon accumulation model which named multi-element matching (T-CDMS) for prediction for favorable hydrocarbon reservoirs area. Hydrocarbon reservoirs formed at early stage will be adjusted, reconstructed and destroyed because of multi-stages tectonic events, which mainly due to intensity of tectonic events, time of tectonic events, times of tectonic events, and caprocks properties when tectonic events happened, and thus established remaining resources potential assessment model of multi-stages tectonic events after hydrocarbon reservoirs formation, which can be used for prediction the remaining resources potential in the favorable exploration area. The formed hydrocarbon reservoirs show the late stage hydrocarbon accumulation effect after reconstruction, and the same time, facies and potential coupling controlled hydrocarbon reservoirs formation and distribution, the two functions can be used for prediction of the favorable exploration target and further more point out the potential favorable exploration target.

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庞雄奇,周新源,姜振学,王招明,李素梅,田军,向才富,杨海军,陈冬霞,杨文静,庞宏.2012.中国西部叠合盆地油气藏形成、演化与分布预测[J].地质学报,86(1):1-103.
Pang Xiongqi, ZHOU Xinyuan, JIANG Zhenxue, WANG Zhaoming, LI Sumei, TIAN Jun, XIANG Caifu, YANG Haijun, CHEN Dongxia, YANG Wenjing, PANG Hong.2012. Hydrocarbon reservoirs formation, evolution and distribution in the superimposed basin, Western China[J]. Acta Geologica Sinica,86(1):1-103.

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  • 收稿日期:2010-11-15
  • 最后修改日期:2010-11-15
  • 录用日期:2011-08-20
  • 在线发布日期: 2012-01-06
  • 出版日期: