pull-apart basin的意思|示意

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；

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 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。

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。

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。

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负花状构造及其有关构造运动形迹分析的基础上，进一步提出方正断陷是走滑—拉分形成的断陷盆地。