地质科技情报
地質科技情報
지질과기정보
GEOLOGICAL SCIENCE AND TECHNOLOGY INFORMATION
2010年
2期
63-67
,共5页
排烃史%运聚史%成藏动力学%侏罗系%车拐地区%准噶尔盆地
排烴史%運聚史%成藏動力學%侏囉繫%車枴地區%準噶爾盆地
배경사%운취사%성장동역학%주라계%차괴지구%준갈이분지
hydrocarbon expulsion history%migration and accumulation history%pool-forming dynamics%Jurassic%Che-Guai area%Junggar Basin
准噶尔盆地西北缘车拐地区目前已经在侏罗系发现了多个油气藏,分析这些油气藏形成的过程及其主要控制因素具有重要意义.基于成藏动力学的三维模拟结果表明,侏罗系油气藏的油气来源主要是二叠系风城组和乌尔禾组烃源岩,油气运移路径主要表现为由沙湾凹陷向车排子凸起、中拐凸起方向.从充注时间看,侏罗系八道湾组始于早侏罗世(178 Ma),齐古组始于早白垩世(120 Ma),充注过程一直持续到古近纪末期;白垩纪中期的构造运动使车拐地区的地形向现今的"南低北高"发展,改造了已经形成的圈闭,使此前形成的油气藏重新分配,并向北部重新聚集,从而形成现今侏罗系的油气藏主要分布在车拐地区北部和车排子断裂带附近区域,而在车拐地区南部仅存在一些残余油气藏的格局.
準噶爾盆地西北緣車枴地區目前已經在侏囉繫髮現瞭多箇油氣藏,分析這些油氣藏形成的過程及其主要控製因素具有重要意義.基于成藏動力學的三維模擬結果錶明,侏囉繫油氣藏的油氣來源主要是二疊繫風城組和烏爾禾組烴源巖,油氣運移路徑主要錶現為由沙灣凹陷嚮車排子凸起、中枴凸起方嚮.從充註時間看,侏囉繫八道灣組始于早侏囉世(178 Ma),齊古組始于早白堊世(120 Ma),充註過程一直持續到古近紀末期;白堊紀中期的構造運動使車枴地區的地形嚮現今的"南低北高"髮展,改造瞭已經形成的圈閉,使此前形成的油氣藏重新分配,併嚮北部重新聚集,從而形成現今侏囉繫的油氣藏主要分佈在車枴地區北部和車排子斷裂帶附近區域,而在車枴地區南部僅存在一些殘餘油氣藏的格跼.
준갈이분지서북연차괴지구목전이경재주라계발현료다개유기장,분석저사유기장형성적과정급기주요공제인소구유중요의의.기우성장동역학적삼유모의결과표명,주라계유기장적유기래원주요시이첩계풍성조화오이화조경원암,유기운이로경주요표현위유사만요함향차배자철기、중괴철기방향.종충주시간간,주라계팔도만조시우조주라세(178 Ma),제고조시우조백성세(120 Ma),충주과정일직지속도고근기말기;백성기중기적구조운동사차괴지구적지형향현금적"남저북고"발전,개조료이경형성적권폐,사차전형성적유기장중신분배,병향북부중신취집,종이형성현금주라계적유기장주요분포재차괴지구북부화차배자단렬대부근구역,이재차괴지구남부부존재일사잔여유기장적격국.
Several reservoirs have been found in Jurassic,Che-Guai area, northwest edge of Junggar Basin. Hence, it is of great significance to analyse the formation progress and main controlling factors. The 3D modeling result obtained, based on pool-forming dynamics, shows that the primary sources of reservoirs in Jurassic were the source rock of Permian Fengcheng Formation and Permian Wuerhe Formation, while the primary direction of migration pathways was from Shawan depression to Chepaizi salient and Zhongguai salient. The filling time of reservoirs shows that Jurassic Badaowan Formation started from Early Jurassic(178 Ma) and Jurassic Qigu Formation started from Early Cretaceous(120 Ma).The filling continued until the end of Paleogene.The tectonic movement that occoured in Cretaceous led the topography of Che-Guai area to be "low in the south and high in the north" and reconstructed the traps and the reservoirs formed earlier. The northward migration also caused the present reservoirs of Jurassic to be mainly distributed in the northern part of Che-Guai area or near the Chepaizi fault zone, leaving only some residual reservoirs in the southern part of Chen-Guai area.