• Microstructure and ultramicrostructure of the strike-slip thrust belt in eastern Jiaodong have been studied using both microscopy and TEM.

    应用偏光显微镜和透射电子显微镜方法,进行了胶东东部走滑逆冲构造带显微构造及超微构造研究。

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  • The Luochen Copper Mine is situated at the composite part of the protruding south front of the large scale thrust( slip) nappe and the NNE-trend strike-slip thrust fault in the south edge of Jiuling.

    罗城铜矿区处于九岭南缘大型推(滑)覆构造往南突出的前锋与NNE向走滑冲断带复合部位。

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  • The tectonic boundary between the Yangtze Continent and Qinling orogenic belt is a thrust-strike slip tectonic zone rather than a intracontinental subduction zone.

    扬子大陆与秦岭造山带之间的壳内构造边界不具陆内俯冲性质,而是逆冲推复一走滑构造带。

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  • The ratio of poloidal to toroidal component of mantle convection determined the proportion of seismic energy released in the thrust, normal, or strike-slip earthquakes.

    地幔对流的垂直运动与水平运动分量的比率,决定了逆冲、引张与走滑型强震的能量释放份额。

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  • The focal mechanism is mainly left-lateral strike-slip, with a small thrust component.

    震源机制主要是左旋走滑,带有很小的逆冲倾滑分量。

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  • This paper considers that Aerjin Mountain strike-slip fault structure is a huge tectonic zone with the property of left active anticlockwise and thrust nappes and ductile shear zone.

    该文认为,阿尔金山走滑断裂构造是一巨型左行左列走滑断裂兼逆冲推覆和韧性剪切性质的断裂构造带。

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  • Thrust- faults and strike-slip faults are the major structures in the studied area.

    逆冲断层及边界走精断层是区内主要控矿构造。

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  • The said fracture zone is composed of a series of ductile and brittle thrust faults, strike-slip faults and blocks as well as tectonic slices.

    该带由韧性又脆性冲断层、平移断层,以及各种岩块、构造岩片等组合而成。

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  • The foreland thrust belt has complex and various structural styles. Besides the large-scale reverse faults, there are a series of north-west strike-slip faults.

    准噶尔盆地西北缘前陆冲断带构造样式复杂多样,除规模较大的逆断层外,还发育一系列北西向的走滑断层。

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  • It shows sinistral strike-slip movement in western and middle segment, sinistral strike-slip and thrust in eastern segment.

    西段和中段表现为左旋走滑,东段表现为左旋走滑逆冲运动。

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  • The observations of seismologists at the BGS suggest both things: more thrust in the SW, nearer the epicentre, and more strike-slip toward its direction of propagation, the NE.

    地震学家在BGS上的观测暗示出两件事:在接近于震源中心部位的西南方向上有更大的推力;在东北方向的传播方位上有更大的碰撞滑动。

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  • The observations of seismologists at the BGS suggest both things: more thrust in the SW, nearer the epicentre, and more strike-slip toward its direction of propagation, the NE.

    地震学家在BGS上的观测暗示出两件事:在接近于震源中心部位的西南方向上有更大的推力;在东北方向的传播方位上有更大的碰撞滑动。

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