• 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 structural style found in the basin includes imbricated thrust zone, trapdoor structure, drag fold, listric fault, rollover anticline, horst-graben structure and the like.

    盆地发育多种构造样式主要有瓦状断层、滚板构造牵引褶皱形正断层、滚动背斜、“垒一”构造

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  • Hefei basin is a Mz-Cz residual basin generated from common action by Dabie orogen and Tanlu (TanchengLujiang) fault zone.

    合肥盆地大别造山带庐断裂带共同作用产生的中新生代残留盆地。

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  • The normal fault zone with NEE trending are cut by some NNW faults with left-lateral dislocation in the north of the basin.

    盆地北缘东东向正断层北北西向断裂旋错动。

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  • Weibei basin is a Mesozoic-Cenozoic basin developed in the Tanlu fault zone.

    潍北盆地发育庐断裂带内中、新生代盆地。

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  • The overthrust fault zone and foreland basin in Southwestern Tarim is favorable areas for petroleum exploration. But the research and exploration degree here are still low.

    塔西南山前冲断带及其前陆盆地系统一个油气勘探前景较好的地区目前对地区的研究程度勘探程度比较低。

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  • Tertiary pull apart basin named Laolongwan basin was found in the Haiyuan fault zone.

    海原断裂带内部发现一个第三纪盆地命名为老龙湾拉分盆地。

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  • In fact, the volcanic rock zone is a fault subsidence basin zone in tectonic sense.

    构造意义而言火山实质上盆地带。

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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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  • Depositional characteristics of the Hefei basin indicated a good coupling with evolution of the Tan-Lu fault zone to the east of the basin.

    合肥盆地沉积作用与其缘的庐断裂带演化有着良好耦合关系

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  • Hefei basin, closely near to the west of Tan-lu fault, is a Mes-Cenozoic compound superposition basin. Its generation and evolution have a close relationship with the activities of Tan-lu fault zone.

    合肥盆地紧邻断裂带苏皖西侧发育典型新生代复合叠加盆地,合肥盆地的成生、演化郯庐断裂带活动有着密切联系

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  • The Kebai fault zone is one of most prolific areas in Junggar Basin. But its oil source is still poorly understood.

    断裂带准噶尔盆地油气聚集最为丰富地区一直是悬而未决的问题。

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  • Meticulous depiction of internal structure of fault zone inside basin is great significant in analysis the role of fault in the oil and gas migration and accumulation.

    精细刻画盆地内部断裂带内部结构特征对于分析断裂油气运聚中所作用具有重要意义。

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  • The Yumen fault, as a part of the northern Qilianshan fault zone, is a branch of the south-margin fault of the Jiuquan basin and also the boundary of the second-order structural element in this basin.

    玉门断裂祁连山北缘断裂带组成部分属于酒西盆地南缘断裂带的一支,是酒西盆地内二级构造单元的边界

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  • A Tertiary pull apart basin named Laolongwan basin was found in the Haiyuan fault zone.

    海原断裂带内部发现一个第三纪盆地命名为老龙湾拉分盆地。

    youdao

  • A Tertiary pull apart basin named Laolongwan basin was found in the Haiyuan fault zone.

    海原断裂带内部发现一个第三纪盆地命名为老龙湾拉分盆地。

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