印支期 meaning in Chinese
indo-chinese epoch
Examples
- Sedimentary characteristics and provenance analysis of indo - chinese epoch in the southwest edge of ordos basin
鄂尔多斯盆地西南缘印支期沉积特征及物源 - Indosinian nappe structure and its hydrocarbon significance in hefei basin and north huaiyang tectonic zone
合肥盆地与北淮阳构造带印支期的推覆构造及其油气意义 - 7 . the dabie orogenic belt is of transformation and superposition character . its new superimpose
Ne向郯庐断裂系的大型平移作用叠加在原来印支期消减带之上，产生新的俯冲。 - Camp belong to the south qinling orogenic belt middle segment palaeozoic strench basin fold indo - chinese epoch drape north part , and belong to the miliangchuan schiefer
矿区所在部位属南秦岭造山带中带古生代伸展盆地叠加印支期冲褶带的北部，隶属于米粮川逆冲岩片。 - The qiongzhong granite should have been formed at orogenic relaxing stage after the peak of indosinian orogeny , and the danxian granite were formed at the latest orogenic phase
琼中岩基可能形成于“印支期”碰撞造山运动峰期后的松弛阶段，而儋县岩基则可能形成于造山运动的结束阶段。