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 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 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.
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。
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 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;