云南东部中上元古界的界线长期以来被置于晋宁运动所造成的不整合界面上。
The boundary between Middle and Upper Proterbzoic Erathem in East Yunnan was put on the unconformity interface led by the Jinning Movement for a long time.
基底与盖层之间的高角度不整合界面，系武陵造山运动的记录。武陵运动与华北地台的吕梁运动相当。
The unconformity between the basement and the cover is the record of Wuling orogeny equal to Luliang orogeny of Huabei platform.
在巴楚地区，影响平均速度变化的主要因素是大的构造运动形成的多角度不整合界面和断距较大的断层。
In Bachu Area, the major factor of impacting average velocity variety is multi big Angle unconformity interface that heave tectonic movement formed and big heave fault.
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