现代地质
現代地質
현대지질
GEOSCIENCE-JOURNAL OF GRADUATE SCHOOL CHINA UNIVERSITY OF GEOSCIENCES
2013年
5期
1081-1088
,共8页
郭继刚%李建华%庞雄奇%向才富%姜福杰%王鹏威
郭繼剛%李建華%龐雄奇%嚮纔富%薑福傑%王鵬威
곽계강%리건화%방웅기%향재부%강복걸%왕붕위
排烃效率%排烃门限%烃源岩%侏罗系%下部成藏组合%准噶尔盆地南缘
排烴效率%排烴門限%烴源巖%侏囉繫%下部成藏組閤%準噶爾盆地南緣
배경효솔%배경문한%경원암%주라계%하부성장조합%준갈이분지남연
expulsion efficiency of hydrocarbon%hydrocarbon-expulsion threshold%source rock%Jurassic%the below oil-reservoir combination%southern margin of Junggar basin
准噶尔盆地南缘下部成藏组合勘探日趋重要,其主力烃源岩生烃潜力和排烃效率的研究亟待加强。根据排烃门限理论,利用生烃潜力法建立了准噶尔盆地南缘侏罗系烃源岩的生、排烃模式,并计算了烃源岩的生烃量、排烃量和排烃效率。研究表明,准噶尔盆地南缘侏罗系泥质烃源岩和煤层的排烃门限对应的镜质组反射率均为0.7%。侏罗系烃源岩的总生烃量为3973.84×108 t,总排烃量为1402.71×108 t,其中八道湾组烃源岩排烃量占总排烃量的69.85%。准噶尔盆地南缘侏罗系烃源岩的平均排烃效率为35.30%,不同层系不同岩性烃源岩,其排烃效率明显不同,泥质烃源岩排烃效率远大于煤层。综合分析认为,准噶尔盆地南缘侏罗系烃源岩生、排烃量大,排烃效率较高,下部成藏组合以侏罗系烃源岩为主力烃源岩,具有良好的资源潜力。
準噶爾盆地南緣下部成藏組閤勘探日趨重要,其主力烴源巖生烴潛力和排烴效率的研究亟待加彊。根據排烴門限理論,利用生烴潛力法建立瞭準噶爾盆地南緣侏囉繫烴源巖的生、排烴模式,併計算瞭烴源巖的生烴量、排烴量和排烴效率。研究錶明,準噶爾盆地南緣侏囉繫泥質烴源巖和煤層的排烴門限對應的鏡質組反射率均為0.7%。侏囉繫烴源巖的總生烴量為3973.84×108 t,總排烴量為1402.71×108 t,其中八道灣組烴源巖排烴量佔總排烴量的69.85%。準噶爾盆地南緣侏囉繫烴源巖的平均排烴效率為35.30%,不同層繫不同巖性烴源巖,其排烴效率明顯不同,泥質烴源巖排烴效率遠大于煤層。綜閤分析認為,準噶爾盆地南緣侏囉繫烴源巖生、排烴量大,排烴效率較高,下部成藏組閤以侏囉繫烴源巖為主力烴源巖,具有良好的資源潛力。
준갈이분지남연하부성장조합감탐일추중요,기주력경원암생경잠력화배경효솔적연구극대가강。근거배경문한이론,이용생경잠역법건립료준갈이분지남연주라계경원암적생、배경모식,병계산료경원암적생경량、배경량화배경효솔。연구표명,준갈이분지남연주라계니질경원암화매층적배경문한대응적경질조반사솔균위0.7%。주라계경원암적총생경량위3973.84×108 t,총배경량위1402.71×108 t,기중팔도만조경원암배경량점총배경량적69.85%。준갈이분지남연주라계경원암적평균배경효솔위35.30%,불동층계불동암성경원암,기배경효솔명현불동,니질경원암배경효솔원대우매층。종합분석인위,준갈이분지남연주라계경원암생、배경량대,배경효솔교고,하부성장조합이주라계경원암위주력경원암,구유량호적자원잠력。
The below oil-reservoir combination in the southern margin of Junggar basin is playing an important role in the hydrocarbon exploration,thus it is necessary to focus our attention on the research on hydrocarbon potential and expulsion efficiency of hydrocarbon of chief source.In this paper,based on the theory of hydrocar-bon-expulsion threshold,models of hydrocarbon generation and expulsion of the Jurassic source rocks were es-tablished and their quantity of hydrocarbon generation and expulsion,expulsion efficiency of hydrocarbon were calculated by using the hydrocarbon-generation potential method.The results showed that the vitrinite reflec-tance corresponding to hydrocarbon-expulsion threshold of both mudstone and coal seam is 0.7%.The total hy-drocarbon generation quantity and the total hydrocarbon expulsion quantity of the Jurassic source rocks are 3,973.84 ×108t and 1,402.71 ×108t respectively.Of all the hydrocarbon expulsion quantity,69.85 percenta-ges of them were expulsed by the source rocks in Badaowan Formation.The average hydrocarbon expulsion effi-ciency of Jurassic source rocks is 35.30%in the southern margin of Junggar basin.The hydrocarbon expulsion efficiency of source rock with different series of strata and different lithology is obviously different.The hydrocar-bon expulsion efficiency of mudstone is much higher than that of coal seam.In general,source rocks in the Ju-rassic have generated and expulsed large amounts of hydrocarbons,and the expulsion efficiency of hydrocarbon is quite high,indicating a promising resource prospect of the below oil-reservoir combination in the southern margin of Junggar basin.