鄂尔多斯地块西缘构造带的主要形式是逆冲推覆构造。
The main type of the west margin tectonics belt of the Ordos massif is characterised by thrust nappe.
分析了鄂尔多斯地块南部和渭河盆地构造的空间分布特征。
The space distribution characteristics of structures from topography and landform of the south part of Ordos block and Weihe basin are analyzed.
受甘青块体顺时针旋转运动的藕合影响，鄂尔多斯地块表现为逆时针旋转运动；
Acted by Gansu-Qinghai rotating block at the NW Liupanshan range, the Erdos block takes anti-clockwise rotation;
鄂尔多斯地块与阿拉善地块间有一个具有拐折结构的剪切变形带，鄂尔多斯地块的西北角和东南缘处于NNW -SSE方向的受拉伸状态。
Junction zone between the Ordos and Alxa block is a shear zone with sections of variable trend. The northwestern and southeastern marginal region of the Ordos is under NNW SSE extension.
鄂尔多斯地块与阿拉善地块间有一个具有拐折结构的剪切变形带，鄂尔多斯地块的西北角和东南缘处于NNW -SSE方向的受拉伸状态。
Junction zone between the Ordos and Alxa block is a shear zone with sections of variable trend. The northwestern and southeastern marginal region of the Ordos is under NNW SSE extension.
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