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thrust fault相关的网络例句

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与 thrust fault 相关的网络例句 [注:此内容来源于网络,仅供参考]

Selibuya Fault has typical double structures and is composed of deep thrust fault and shallow and nappe thrust fault.

色力布亚断裂具有典型的双重结构,由深层逆冲断裂与浅层逆冲推覆断裂组成。

Firstly,we should discuss the definition of thrust belt,thrust fault,overthrust belt, reversed fault and overthrust fault and their differences,and then analyze the causes of formation and mechanisms as well as the tectonic background.

如何看待冲断带油气勘探,首先要讨论冲断带、冲断层、掩冲带、逆断层、逆掩断层的定义及其差异,然后分析冲断带的成因机制和形成的大地构造背景,冲断带油气勘探的兴衰历史。

Firstly,we should discuss the definiton of thrust belt,thrust fault,overthrust belt, reversed fault and overthrust fault and their differences,and then analyze the causes of formation and mechanisms as well as the tectonic background.

如何看待冲断带油气勘探,首先要讨论冲断带、冲断层、掩冲带、逆断层、逆掩断层的定义及其差异,然后分析冲断带的成因机制和形成的大地构造背景,冲断带油气勘探的兴衰历史。

Based on the analysis of the major pattern of the faults in Tazhong, the feature and the patterns of the fault system was revealed. The patterns of flower structure, imbricated thrust ,Y-fault, back to back thrust fault, and ramp were developed in this zone.

剖面上断裂主要表现为基底卷入式的较高角度逆冲断裂,主要逆断裂均发育有与其背冲的伴生断层,构成&两断夹一隆&的花状构造样式;平面上发育近北西、近北东及近东西向三组断裂。

Based on the field study of fault outcrops and landform deformations ,combining with TL and 14C ages,it is concluded that the north marginal fault of the Yumu mountain is a thrust with left-lateral slipping and the east marginal fault is a thrust with right-lateral slipping,and the Yumu Mountain developed from the resulting uplifting of the Yumu Mountain block along these faults.

根据野外断层露头和地貌体的变形测量和分析,本文认为榆木山北缘断层是一条具有左旋位移的逆断层,东缘断层是一条具有右旋位移的逆断层,这两条断层在全新世期间都有明显的活动。榆木山的发育是沿着北缘断层和东缘断层的逆活动,造成山体内地块叠加变形的结果。

The thrust washer and thrust collar have complementary configurations that maintain the thrust washer in position on the shaft adjacent the thrust collar.

止推垫圈(76)和止推轴环(70)具有互补性的构造,能够将止推垫圈(76)与止推轴环(70)相邻地保持在所述电动机轴上适合的位置中。

Normal Fault Flash Animation 正向断层Flash动画 thrust fault - a dip-slip fault in which the upper block, above the fault plane, moves up and over the lower block.

冲断层 -断层平面上面的岩体向上运动并压住下面的岩体的一种倾滑断层。

Finally, the controlling role of structure to sedimentary was analyzed. It is showing that time-transgressive different structural zone developed different sedimentary system; the thickness of sedimentary formation and lithic facies were different on the simultaneous lateral layer of growth fault; the expansive orientation of sedimentary system was controlled by the strike of fault; the sedimentary system developed differently became of the tectonic activity was differently; step thrust slip fault can built-up multistage fault fans.

最后分析构造对沉积的控制作用,主要表现在:不同时期不同的构造带发育不同的沉积体系;生长断层造成断层两侧同期地层沉积厚度与岩相的明显差异;断层的走向控制沉积体系的展布方向;构造活动导致沉积体系的发育有显著的差异;阶梯式逆冲断层可形成多级断崖扇。

In the section,the North Block-faulted Belt developed three sets of fault system s including lower thrust fault system ,upper detachment fault system and top normal fault system .

在剖面上,该区发育3套断层系统,即下部冲断层系统、上部滑脱断层系统和顶部正断层系统。

On the basis of seismic data and regionally electromagnetic sounding data in zhanhe fault depression and Jiayin fault depression,combining the drilling data of Jia-D1 well and Jia-D2 well,beginning from geologically constructional character of the basin and its circumambience,integrating the up-to-dade theories of sequence stratigraphy home and abroad,the thesis firsthy indudes the constructional pattern,the process of constructional evolvement,the process of sedimentary evolvement,the character of lava\'s groming and the geological character of oil\'s producing,depositing and coveringThe tectonic framwork of Zhanhe fault depression is two sags and one uplift , the tectonic framwork of Jiayin fault depression is three sags and two uplifts, the strikes of structures are the north north-east, early it is a fault depressions and later becomes a depression s so this basin is faulted depressed basins.

涉及隐私,隐去***论文是以沾河断陷、嘉荫断陷地震资料及区域电磁测深资料为基础,结合嘉D1、嘉D2井钻井资料,从盆地及其周边的地质构造特征出发,结合国内、外最新层序地层学理论,首次总结了沾河—嘉荫断陷构造格式、构造演化过程、沉积演化过程、火山岩发育特征和生储盖石油地质特征。沾河断陷表现为两凸夹一凹的构造格式,嘉荫断陷表现为三凸夹两凹,构造走向均为近北北东向,早期表现为断陷特征,晚期表现为坳陷特征,为断、坳复合型盆地。

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