鄂尔多斯地台

用GPS方法与地质学方法得到的鄂尔多斯相对于蒙古地台的旋转参数相同，证明鄂尔多斯自晚新生代以来的运动是稳定的。

The rotation parameters of Ordos block relative to Mongolia platform obtained by GPS method are the same as those acquired by geological method , which indicate that the motion of Ordos block has been stable since late Kainozoic .

鄂尔多斯地区位于华北地台西部，处于东西构造域的交接部位，是我国重要的煤、石油、天然气聚集场所之一。

Ordos which located in the western of Huabei area and intersection point of west and east structual domain is an important gas and coal sinks in china .

根据鄂尔多斯块体及周围地区的GPS数据，计算了鄂尔多斯相对于蒙古地台和欧亚板块的旋转参数，表明鄂尔多斯相对于蒙古地台和欧亚板块存在逆时针旋转。

On the basis of the GPS data observed on Ordos block and its peripheral regions , the rotation parameters of Ordos block relative to Mongolia platform and Eurasia plate are calculated , which prove the counterclockwise rotation of Ordos block relative to Mongolia platform and Eurasia plate .