Tertiary pull apart basin named Laolongwan basin was found in the Haiyuan fault zone.
在海原断裂带内部发现一个第三纪拉分盆地，命名为老龙湾拉分盆地。
A Tertiary pull apart basin named Laolongwan basin was found in the Haiyuan fault zone.
在海原断裂带内部发现一个第三纪拉分盆地，命名为老龙湾拉分盆地。
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.
从渤海湾盆地的中、新生代构造演化分析，渤海湾盆地是一个新生代早第三纪始新世形成的走滑拉分盆地。
The Baise basin is a typical pull-apart basin that was formed in Tertiary Period.
百色盆地是一典型的第三纪走滑拉分盆地。
Jiaolai basin is a strike-slip and pull-apart basin controlled by the Yishu Fault Belt and Wulian -jimo-muping Fault.
胶莱盆地是中生代走滑拉分盆地，其形成与发育受到沂沭断裂和五莲-即墨-牟平断裂的控制。
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.
南秦岭新生代房县盆地是北西向安康竹山房县左旋走滑断裂构造带东南端拉分盆地。
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;
胶莱走滑拉分盆地层序特征表现为：（1）靠近走滑断层的区域发育浅水型层序，而远离走滑断层的区域发育深水型层序；
During the Late Jurassic, this pull-apart basin reversed resulting from the eastward compression of the Alxa Block.
在晚侏罗世，该地区的拉分盆地由于受到阿拉善地块的东向挤压而反转。
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.
拉分盆地指沿着走滑断裂带弯曲部位，由于拉张而产生的地形上的低洼处， 多形成于走滑断裂带次级断裂的间列部位。
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—五峰山和黄尖丘—新场两地区形成正性的走滑隆升区，其相应中间地带则显示了负性拉分拗陷作用，发育了大奇山拉分盆地。
Resulting from the sinistral displacement of the NE-trending fault, there is a pull-apart basin in the Feng Zhou area.
由于北东向断层的左行走滑，在丰州一带生成拉分盆地。
The extensional structures in Mesozoic-Cenozoic inside the Shanxi Plateau are mainly characteristic of pull-apart basin development, similar to the ones in front of the Taihang Mountains.
山西高原内部中新生代拆离构造特征与太行山前类似，伸展构造以拉分断陷为主。
The extensional structures in Mesozoic-Cenozoic inside the Shanxi Plateau are mainly characteristic of pull-apart basin development, similar to the ones in front of the Taihang Mountains.
山西高原内部中新生代拆离构造特征与太行山前类似，伸展构造以拉分断陷为主。
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