Faults which show both dip-slip and strike-slip motion are known as oblique-slip faults.

断层既有倾滑又有走滑运动特征的被称为斜滑断层。

Faults which move along the direction of the dip plane are dip-slip faults and described as either normal or reverse , depending on their motion .

沿倾角方向移动的断层称为倾滑断层，并按他们的运动方向分别描述为正向或逆向。

The style of the active fault is normal-dip-slip accompanied by sinistral stike-slip. The active fault had many times of activity during Holocene.

全新世时期该断裂有多次活动，活动方式以具左旋性质的正倾滑为主。

In the Xindukushi region, the focus offsets are mainly the form of dip-slip thrusts, the elevation angles of axis T almost vertical;

兴都库什地区震源断错以倾滑道断层为主，T轴仰角几乎垂直。