准噶尔盆地腹地石油地质特征与找油领域

1993年 14卷 第No.1期
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PETROLEUM GEOLOGICAL CHARACTERISTICS AND OIL PROSPECTS IN CENTRAL JUNGGAR BASIN
李溪滨 买光荣 况军 贾希玉
Li Xibing Mai Guangrong Kuang Jun Jia Xiyu
准噶尔盆地腹地为前寒武系结晶基底和泥盆、石炭系浅变质基底,分6个构造-沉积演化阶段,具5凸4凹共9个二级构造单元,下二叠统风城组、上二叠统下乌尔禾组和侏罗纪煤系为3套烃源层,有三套油气生储盖组合,莫索湾凸起、白家海凸起、三南凸起和中拐-达巴松凸起是有利的油气聚集区。
The basement of the hinderland of Junggar Basin consists of two layers,the Pre-cambrian crystalline and the Devonian-Carboniferous slightly metamorphic basement.From Permian to Quaternary,the hinderland experienced six structural-sedimental stages:1.platform marine basin;2.foreland marine basin;3.taphrogenic remnant marine basin;4.depressed continental basin;5.oscillation continental basin and 6.constriction continen-tal basin.Nine secondary structural units can be divided and Zhongguai-Dabasong,San-nan,Baijiahai,Muosuowan uplifts are favourable for hydrocarbon accumulation.The Permian Fengcheng(P∫),lower Wuerhe(Pω)Formations and the Jurassiccoal measures(J)are source beds in the area.Triassic-Permian traps formed in lateHercynian—Indo-China epoch received mainly oil and gas from Permian source rocksand belong to allogenic type;Jurassic traps formed in early Yenshan epoch received oiland gas from Permian and Jurassic source rocks,and belong to autogenetic and combinedtypes.
准噶尔盆地; 构造-沉积演化阶段; 烃源岩; 二叠系; 侏罗系; 油气远景评价;
10.11743/ogg19930104