The Jurassic petroleum in the Well Shishen 1, Lenghu no. 3 Oilfield, north Qaidm Basin, is much likely a typical feature of the pitch sealing fault body accumulation type.
柴达木盆地北缘的冷湖三号石深1井侏罗系油气藏可能是典型的沥青封堵型断层体油气藏。
The structural pattern of the normal fault assemblage that occurred in the Early and Middle Jurassic may have initiated some small-scale petroleum and gas pools.
早、中侏罗世形成的正断层组合构造样式，可形成一些小规模油气藏。
Early Jurassic to early cretaceous basin group of western Liaoning is a distinguished group of fault basin.
辽西地区的早侏罗世—早白垩世盆地群是一类颇具特色的断陷盆地群。
In addition to the piedmont zone, the Jurassic strata in southwestern Tarim were also developed in a series of fault-controlled lake basins.
塔西南地区侏罗纪地层除发育在山前外，还发育了一系列受断层控制的湖盆。
The Early-Middle Jurassic strata were probably deposited in an extensional basin above the Lapeiquan fault.
早中侏罗世地层可能为拉配泉断裂之上的伸展盆地沉积。
This has very important significance for the gas reservoir research of the Jurassic volcanic rocks in the Yingshan Fault Depression of the Songliao Basin.
这对松辽盆地莺山断陷侏罗系火山岩储气层的研究具有十分重要的意义。
Uplift in the southwestern Qaidam Basin led to the migration of Middle Jurassic strata to the north and west, and resulted in the formation of inverted haft-graben fault basin.
柴西南隆升导致中侏罗世地层向北、北东迁移，并出现反向箕状断陷盆地。
The fault subsidence lacustrine died out in late-Jurassic and damp type fan, braided stream and meander river sedimentary sequence was formed.
上侏罗统为断陷消亡期沉积，形成湿型扇—辫状河—曲流河沉积序列。
By means of 1/50000 negional surveying, it has been established that Zongbieli marginal fault control of thebasin sedimentation and the distribution range of Jurassic System.
通过1：5万区域地质调查工作，基本查明了侏罗系的分布范围及宗别立边界断裂对盆地沉积作用的控制。
Faults are vertically subdivided into deep fault system and shallow fault system by the bottom of Jurassic Formation at Wuxia area.
根据地震解释结果，本区断裂系统在纵向上具有明显的分层性，以侏罗系底为界，划分为深部和浅部两套断裂系统。
There is a normal deposition sequence stratigraphy beneath the lower wall of over-thrust fault, such as Jurassic, Triassic, Permian-Carboniferous, Cambrian-Ordovician system.
在逆冲断裂的下盘，是一套正常沉积层序的地层，分别为侏罗系、三叠系、石炭—二叠系、寒武—奥陶系等地层。
There is a normal deposition sequence stratigraphy beneath the lower wall of over-thrust fault, such as Jurassic, Triassic, Permian-Carboniferous, Cambrian-Ordovician system.
在逆冲断裂的下盘，是一套正常沉积层序的地层，分别为侏罗系、三叠系、石炭—二叠系、寒武—奥陶系等地层。
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