• According to the analysis of Mesozoic and Cenozoic tectonic evolution, Bohai Bay basin is a strike slip pull apart basin formed in the Cenozoic Eocene epoch.

    渤海湾盆地新生代构造演化分析渤海湾盆地一个新生代早第三纪始新形成盆地。

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  • Based on the negative flower shaped structure and its relative structural movement track in Fangzheng area, this paper suggests that Fangzheng rift is a rifted basin formed by strike slip pull apart.

    本文通过对方正地区所发现的构造及其有关构造运动形迹分析的基础上,进一步提出方正滑—形成盆地

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  • Jiaolai basin is a strike-slip and pull-apart basin controlled by the Yishu Fault Belt and Wulian -jimo-muping Fault.

    胶莱盆地中生代走滑拉分盆地,形成发育受到沂沭断裂五莲-即墨-牟平断裂的控制

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  • The Jiaolai strike-slip pull-apart basin is characterized by: 1 shallow-water sequences along the strike-slip faults and deep-water sequences far from the strike-slip faults;

    胶莱盆地特征表现为:(1)靠近走滑断层的区域发育浅水型层远离走滑断层的区域发育深水型层序;

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  • Huanushan - Wufenshan and Huangjianqiu -Xinchang formed positive strike -slip up-warping region, middle belt shown negative down warping, developed Daqishan pull -apart basin.

    花牛山五峰山黄尖丘—新场两地区形成性的走滑隆升区,其相应中间地带显示了陷作用,发育了大奇山拉分盆地

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  • The pull-apart basin formed around the steps of the strike-slip fault refers to a low terrain area due to tensile force from the fault.

    盆地沿着走断裂带弯曲部位,由于拉张而产生地形上的低洼处, 多形成于走滑断裂带次级断裂的间列部位。

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  • The study shows that volcanic activity in Xiangshan volcanic basin may be divided into two cycles, and its emplacement is controlled by strike slip pull apart process originated from the deep regiona.

    研究表明 ,相山火山盆地火山活动划分两个旋回就位受制于区域断裂的走分作用。

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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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  • 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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