• In this paper, a method, the uniform slip method, estimating average slip rate along surface trace of strike slip fault zone by historical earthquake data is offered.

    本文介绍并完善了作者提出的一种根据历史地震资料估计断裂带地表断层平均滑动速率方法:“均一滑动”。

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  • In Longling fault zone and the area north to it, the direction of maximum compressional stress is near NS or NNW, the stress regime is of strike slip type.

    龙陵断裂带及其以北的局部地区最大主压应力方向南北北北西,应力结构滑型。

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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.

    该文认为阿尔金山断裂构造巨型行左列走滑断裂兼冲推覆韧性剪切性质断裂构造

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  • The secular GPS crustal deformation image has reflected the relatively complete left lateral strike slip movement of this active fault zone.

    趋势GPS地壳形变图像反映条活动断裂带相对完整活动

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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.

    扬子大陆秦岭造山带之间壳内构造边界不具俯冲性质,而是逆冲推复走滑构造

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  • The left-lateral strike-slip movement of the Zhongwei fault zone since late Pleistocene caused the differentiation of preexisting overthrust faults in the zone.

    青藏高原东北缘中卫断裂带更新世以来旋走运动中,先存的挤压逆掩、逆冲断裂带发生了分化

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  • The main fracture of the western margin fault zone of the South China Sea is originated from the Mesozoic basement fault, continuously developed into dextral strike-slip fault zone in Cenozoic.

    南海西断裂带断裂一条形成于中生代基底断裂新生代持续活动扩展右行走活动断裂带

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  • Differential strain between both terrains was accommodated across the Wenchuan-Mouwen ShearZone, which developed during D_3 as a sinistral strike-slip zone.

    两个地区的差异应变发育D_3的汶川-茂汶剪切带容纳

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  • Detailed analyses of satellite images and field investigation have revealed that the active Kaidu River fault zone on the southern margin of the basin is a strike-slip fault zone.

    详细卫星图像分析野外调查表明活动断层(开都河断层)主要分布盆地南缘,具典型的走断层特征。

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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.

    韧性脆性断层平移断层,以及各种岩块、构造岩等组合而成。

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  • Tanlu strike-slip fault zone had experienced several phases of movement, exerting strong influence and control upon the hydrocarbon pooling within the zone.

    庐走断裂带经历活动影响控制走滑断裂带内的油气成

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  • According to lots of field works, two phases of sinistral strike-slip ductile shear belts were found in the Tan-Lu fault zone.

    大量野外工作发现郯庐断裂带存在早、晚韧性剪切

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  • It is significant to study the characters of the strike-slip structures for trap prediction and prediction of rules of hydrocarbon accumulation along the strike-slip fault zone.

    研究构造发育特征对于预测圈闭分布以研究油气富集规律具有重要意义。

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  • The Hanling-Pianling strike-slip fault zone is an important fault zone of the east of Liaoning, and a secondary fault at the east wall of the Tan-Lu fault zone in China.

    岭—偏岭平移断裂带位于辽宁东部,是中国东部断裂一个次级断裂

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  • The unevenness of crystalline basement is found to be the governing factor for forming the NNE-striking blind basement strike-slip zone and the strike-slip tectonics in the Cenozoic platform cover.

    构造样式、沉积特征、断层组合等方面探讨了黄骅盆地海岸线两侧右旋走滑构造变形存在,指出结晶基底的不均匀NNE基底隐伏走滑形成新生代盖层走滑构造产生控制因素

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  • It indicates that two dynamical mechanisms of mantle diaper and right-lateral strike slip in deep faulted zone lead tectonic dynamics model evolved in Cenozoic stress field of Dongpu depression.

    提出了地幔断裂带右旋走位移两种动力机制联合作用主导东濮凹陷新生代应力场演化构造动力学模式

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  • The Fangxian basin of Cenozoic era of south Qinling is a pull-apart basin at the southeastern end of the Ankang-Zhushan-Fangxian NW-trending left-lateral strike-slip fault zone.

    秦岭新生代房县盆地北西向安康竹山房县左旋走断裂构造东南端拉分盆地。

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  • Bozhong 34-1 complex fault-blocks zone is located in Yanlu strike-slip fault zone. Affected and controlled by the strike-slip fault zone, faults are developed.

    渤中34 - 1浅层复杂处于庐走滑断裂带内,其影响控制该区断层较发育。

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  • Bozhong 34-1 complex fault-blocks zone is located in Yanlu strike-slip fault zone. Affected and controlled by the strike-slip fault zone, faults are developed.

    渤中34 - 1浅层复杂处于庐走滑断裂带内,其影响控制该区断层较发育。

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