The gliding nappe structure was mainly formed before the late Triassicera, but it was still mobilizing after the...
武功山伸展拆离滑覆构造主要形成时期在晚三叠世之前，但晚三叠世之后仍有活动。
The gliding nappe structure was mainly formed before the late Triassicera, but it was still mobilizing after the late Triass…
武功山伸展拆离滑覆构造主要形成时期在晚三叠世之前，但晚三叠世之后仍有活动。
The gliding nappe structure was mainly formed before the late Triassicera, but it was still mobilizing after the late Triassic era.
武功山伸展拆离滑覆构造主要形成时期在晚三叠世之前，但晚三叠世之后仍有活动。
According to regional geology and deep data, the deposit is considered as a gliding nappe system, whose upper and lower shielding layers are sandy mudstone, the middle part is dolomite.
据深部资料结合区域地质特征分析，矿床为一滑覆构造系统。该系统上、下均有砂泥岩作屏蔽层，中间为云岩，形成一个对成矿极为有利的构造封闭系统。
There occurs ductile-brittle gliding-nappe faults in the Proterozoic, new and old cap rocks on the north margin of the depression in the Shidaohe area, Yangzhishao, southern part of Jilin Province.
在吉南样子哨坳陷北缘石道河镇一带，于元古代新老盖层间存在韧—脆性滑覆断层。
There occurs ductile-brittle gliding-nappe faults in the Proterozoic, new and old cap rocks on the north margin of the depression in the Shidaohe area, Yangzhishao, southern part of Jilin Province.
在吉南样子哨坳陷北缘石道河镇一带，于元古代新老盖层间存在韧—脆性滑覆断层。
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