地面地质和各种地球物理资料查明断面是南倾的。

Geological and various geophysical data indicate that the fault plane is inclined to the south.

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西部隆起区结构独特，浅中部与深部结构有别，存在一南倾低阻异常带。

In the west and central profile, the structure of the south Qiangtang depression is similar to the deep structure of the west uplift, featuring a double-layer intracrustal low-resistivity zone.

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南秦岭横丹浊积岩系是一套巨厚的浊流沉积，以向南或南东倾的单斜构造产出。

The Hengdan turbidite sequence is composed of very thick, normal turbidity current deposits. It is marked by a monocline dipping south or southeast.

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