高校地质学报
高校地質學報
고교지질학보
GEOLOGICAL JOURNAL OF CHINA UNIVERSITIES
2013年
3期
552-560
,共9页
黄艳辉%高先志%刘震%林社卿%罗家群%朱颜
黃豔輝%高先誌%劉震%林社卿%囉傢群%硃顏
황염휘%고선지%류진%림사경%라가군%주안
成藏期次%成藏过程%成藏模式%古城油田%泌阳凹陷
成藏期次%成藏過程%成藏模式%古城油田%泌暘凹陷
성장기차%성장과정%성장모식%고성유전%비양요함
hydrocarbon accumulation period%hydrocarbon accumulation process%hydrocarbon accumulation model%Gucheng oilfield%Biyang depression
利用储层流体包裹体和原油地球化学资料,结合钻井地质和测试分析,对泌阳凹陷古城油田的油气来源、成藏期次、成藏过程和成藏模式的研究结果表明,东南深凹区核三下、核三上亚段烃源岩沿着古城油田北西构造抬升方向顺层两期供油,其中廖庄组沉积末期是油气大规模充注成藏时期。核一段沉积末期,泌阳凹陷东南部深凹区核三下亚段烃源岩达到生排烃高峰,油气从深凹(高势区)沿古城三角洲砂体进入古城鼻状构造(低势区),形成一定规模的古油藏;廖庄组末期构造抬升和断层活动,古油藏遭受一定破坏,同时核三上亚段烃源岩达到生排烃高峰,大规模成熟油气沿古城三角洲砂体横穿断层形成断阶式向上聚敛成藏。
利用儲層流體包裹體和原油地毬化學資料,結閤鑽井地質和測試分析,對泌暘凹陷古城油田的油氣來源、成藏期次、成藏過程和成藏模式的研究結果錶明,東南深凹區覈三下、覈三上亞段烴源巖沿著古城油田北西構造抬升方嚮順層兩期供油,其中廖莊組沉積末期是油氣大規模充註成藏時期。覈一段沉積末期,泌暘凹陷東南部深凹區覈三下亞段烴源巖達到生排烴高峰,油氣從深凹(高勢區)沿古城三角洲砂體進入古城鼻狀構造(低勢區),形成一定規模的古油藏;廖莊組末期構造抬升和斷層活動,古油藏遭受一定破壞,同時覈三上亞段烴源巖達到生排烴高峰,大規模成熟油氣沿古城三角洲砂體橫穿斷層形成斷階式嚮上聚斂成藏。
이용저층류체포과체화원유지구화학자료,결합찬정지질화측시분석,대비양요함고성유전적유기래원、성장기차、성장과정화성장모식적연구결과표명,동남심요구핵삼하、핵삼상아단경원암연착고성유전북서구조태승방향순층량기공유,기중료장조침적말기시유기대규모충주성장시기。핵일단침적말기,비양요함동남부심요구핵삼하아단경원암체도생배경고봉,유기종심요(고세구)연고성삼각주사체진입고성비상구조(저세구),형성일정규모적고유장;료장조말기구조태승화단층활동,고유장조수일정파배,동시핵삼상아단경원암체도생배경고봉,대규모성숙유기연고성삼각주사체횡천단층형성단계식향상취렴성장。
The oil resource, hydrocarbon accumulation period, hydrocarbon accumulation process and hydrocarbon accumulation model for Gucheng oil field in Biyang depression were studied using the data of the seismic, geological well measurement, DST, fluid inclusion of reservoir and analysis of petroleum geochemistry. The results show that the source rocks of the upper member and lower member of Eh3 southeast depression provide oil and gas to respective formations, along southwest that is tectonic uplift direction in Gucheng oil field. There are two periods of hydrocarbon accumulation. One key period is in the end of liaozhuang group. At the end of Eh1, the source rock of the lower member of Eh3 southeast depression reached the peak of hydrocarbon generation, and hydrocarbon migrated from southeast depression into structural nose of Gucheng oil field along deltatic sand body, can form a certain scale of fossil oil accumulation. At the end of liaozhuang group, fossil oil accumulation suffered from some degree of destruction due to tectonic uplift and fault activity, and that the source rock of the upper member of Eh3 southeast depression reached the peak of hydrocarbon. Large mature hydrocarbon crossed fault along delta sand body, forming convergent stepladder type of hydrocarbon accumulation model.