三江盆地绥滨坳陷石油地质条件初探

1992年 13卷 第No.2期
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PETROLEUM GEOLOGICAL CONDITIONS IN SUIBIN DEPRESSION
周志祥 迟元林
Zhou Zhixiang Chi Yuanlin
三江盆地是中生代碰撞前陆沉降带上的一个叠合盆地。盆内广泛接受了中生代晚侏罗世—新生代海相-陆相的含煤碎屑岩沉积。绥滨坳陷是盆地西部的一个西断东超的箕状断陷,面积5470km。坳陷具有良好的成油成气地质条件,并普遍见到煤成气显示,有希望获得中小型气田及油田。
Suibin Depression that covers an area of 5470 km in the west part of Sanjiang Basin is a half-graben faulted depression which faulted in the west but overlapped in the east.The NE-strike faults formed in the early stage controlled strip-shape structures,while the NW-strike faults developed in the late stage cut the structures into secondary blocks that composed of one sag,three uplifts and two slopes.The depression has fine source-reservoir-cap rock assemblage and trap conditions.The two source beds of Upper Jurassic developed in marine Dongrong Formation and the nonmarine coal-measures of the Chengzhihe and Muling Formations contain abundant organic matter.Organic carbon con-tents in mudstones are 0.300%-1.675% in Dongrong Formation;0.864%-2.700% in Chengzhihe and Muling Formations,and the ratio of chloroform extract"A"to that are13.43-117.00 mg/g in Dongrong Formation;8.00-50.60 mg/g in mudstone of Chengzhiheand Muling Formations.The organic carbon contents in carbonic mudstone is 5.725%-19.081%.in Chengzhihe and Muling Formation,and the ratio of chloroform extract"A"to that is 2.0′-19.5 mg/g.According to thevitrinite reflectance °,the Dongrong Formation is 0.67%-0.98% and the Chengzhihe and Muling Formations 0.62%-0.92%,all of them have entered into mature stage.The later two formations are mainly gas-generating rocks.Sandstone developed in Upper Jurassic occupies 50% of the total thickness.Its porosity is 1.9%-23.3%,and permeability 0.01×10-1.41×10μm which satisfied the lower limit of the physical property of gas reservoir.The Upper Jurassic mudstone,being thick and laterally distributed stably,is favourable caprock.Besides,the tuff and Creta-ceous volcanic clastic rocks in local places could also be fine caprocks.The trap condition including linear anticline,diapiric structure,syndepositional anticline,lithologic pinch-outand stratigraphic overlap is good too.On the whole,the depression has favourable oil-gas forming condition,and quite a few coal-formed gas showings have been found.
三江盆地; 绥滨坳陷; 侏罗系; 油气远景评价;
10.11743/ogg19920210