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From geometry and forming mechanism, five secondary styles of the extensional-type structural style, including tilted faulted-block, slide faulted-ramp, buried hill draping, gravitative antiform and diapir, were reported.

滑动断阶构主要发育在坳陷的陡坡带,底辟构造常见于坳陷的洼陷带,潜山披覆构造多发育在盆地四周隆起区与洼陷中的潜山带,而重力背形构造大多发育在主断层的下降盘。

In conclusion, through researches of reservoir characteristics, reservoir prediction and the relationship between reservoir and trap, it indicate that Mainan structure and Mopanlaowan buried structure which was in the bottom wall of the fault were the chief exploration and drilling regions of T_1j~2_2~T_1j~2_1 stratum in Dachiganjing structural belt.

总之,通过储层特征、储层预测,以及圈闭与储层的配置等研究,发现麦南构造及断下盘的磨盘老湾潜伏构造应是大池干井构造带嘉二~2~嘉二~1下步重点勘探及井位部署的地区。

Lithologic character of Eogene syste is interbedded sandstone and mudstone primarily, including the thin layer oil shale, Neocene- Quaternary system is set of rivers deposits. Based on this, through the reaserch of ateral correlation and distribution characteristics of every structural layers show that: Paleozoic synthem overall thickness of relatively stable.The residual thickness of Mesozoic synthem is difference in the horizontal, Residues in the horizontal thickness of greater difference, to the greatest thickness achieve to 4500m. Eogene syste has obviously fault depression basin deposition characteristic, the thickness of many sags achieve to 3000 m ,from Neocene, the stratum crosswise mop tended to be stable.

在此基础上,通过对各构造层横向对比以及展布特征的研究表明,古生界构造层整体厚度相对稳定,冷武-奥陶系残留厚度在1200m左右,石炭-二叠系残留厚度在800m左右;中生界构造层残留厚度在横向上差异较大,最大厚度达到4500m,其中,下-中三叠统仅发育于南部小部分地区,最大厚度在1000m以上,侏罗系-下白垩统整体具有南厚北薄的展布特征,南部冠北洼陷厚度最大,达到3500m;新生界古近系具明显的断陷式盆地沉积特征,多个洼陷厚度在3000m以上,新近纪以后地层横向展布趋于稳定。

In northeastern of basin, together with the structural framework of slope belt and the dynamical information of well, we can conclude that the gas reservoir in Taiyuan-early Shihezi formation dominantly belong to protogene depositional gas reservoir under the normal pressure, and the gas favourable reservoir belt was controled by framwork of main sandbody; But in upper Shihezi Formation to Shiqianfeng Formation the gas reservoir show the feature of secondary Tectonic-depositional gas reservoir under the extremely low pressure, and the gas favourable reservoir belt mainly locate in a zone which the low amplitude structure and main sandbody superposed in the slope belt.

5盆地东北部斜坡带构造与钻井生产动态资料的相关分析结果表明,太原组-下石盒子组气藏主体属于正常压力下的原生岩性气藏,其有利含气区带主要受控于主砂体分布格局;上石盒子组-石千峰组气藏则主要为异常低压下的次生构造-岩性气藏,其有利含气区带主要分布在斜坡带低幅度构造与主砂体叠合区。

The Cenozoic activities are dominated in the southern segmentation,with strongly tectonic uplifting and reworking. But the northern segmentation is hosted by Cretaceous uplift?exhumation,with denudating and weakly tectonic reworking in Cenozoic time.

南段是新生代活动的主控区,以强烈地构造抬升和构造改造为主,而北段总体上受制于白垩纪的抬升-剥露,新生代以来主要表现出剥蚀和弱构造改造的特征。

The important anticline and thrust tectonics are described by plenty of first hand materials coming from field surveys, and tectonically redivided by their tectonic features in Kashi depression.

论文用大量的野外第一手资料较详细地描绘了喀什凹陷内主要褶皱冲断构造带的特征,并依据这些构造特征及成因分析重新进行了喀什凹陷的构造区划。

Many gas chimneys were found in the distribution zone of bottom simulating reflector identified from seismic data. The characteristics of gas chimney are biogenetic mud diapirs by analyzing the parameters of interval velocity, fluid potential, mud content and well data.

地震识别出的似海底反射分布区存在大量的气烟囱构造,通过速度、泥岩含量、流体势等属性参数及钻井资料,判断该烟囱构造为有机成因的泥底辟型烟囱构造。

The Middle Hymalaya Movement is the main stage of reverse faults--migration channels and traps development, and also in this stage the Leikoupo Formation petroleum system formed. The advantageous structural traps lie in low steep and low gentle structures in the broad--gentle synclines or in the north and south plunging areas of the high steep structural belts.

喜山中期运动是本区油气运移通道--断层以及圈闭发育的主要时期,也是雷口坡组成气系统形成的主要时期;其有利圈闭多发育于高陡构造带中宽缓向斜内部或高陡构造带南北两侧倾没消失部位的低陡和低缓构造。

This paper presents an algorithm to construct O-O software fault-tree from class-inheritance-relation graph.

文章提出了一个从类的继承关系图构造面向对象软件故障树的构造算法,并且提出了构造多层故障树的设想。

Application of structural geology and rock mechanics, all kinds of geology nature of rock mass which are controlled by joint were discussed, at the same time, the paper analyzed structural trace and its geology influence factors.

运用构造地质学的原理和方法并结合岩体力学理论,描述了研究区受结构面控制的岩体的各种地质属性及其构造环境,本文中构造环境着重于岩体结构面的分析及地应力研究。

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