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本井田构造线主要走向为北东和北北西两组。它们的反接复合形成了大量轴向辗转弯曲的宽缓褶皱及走向辗转亏曲、力学性质复杂和位移方式多变的断裂构造。井田经历的构造演化为纬向系─先北西西系─中新华夏系─后北西西系─北北西系。
The mine field tectonic line mainly to the North East and North North West two groups. Their reverse combination of the formation of a large number of axial rolling broad and gentle fold wrinkles to turn around, the mechanical properties of complex and changing the displacement of the fracture structure. The structural evolution experienced by Ida has been latitudinal-first North-West-Central China-Neocene-West North-West-North-Northwest.