矿石结构主要为泥质结构和显微鳞片泥质结构，构造主要为微层状、板状和致密块状；
The ore has the pelitic and microscale pelitic texture and the micro-bedded, tabular and dense massive structure.
盆地中发育多种构造样式，主要有：叠瓦状冲断层、滚板构造、牵引褶皱、铲形正断层、滚动背斜、“垒一堑”构造等。
The structural style found in the basin includes imbricated thrust zone, trapdoor structure, drag fold, listric fault, rollover anticline, horst-graben structure and the like.
沙丘内部发育有高角度板状交错层理、低角度楔状交错层理等层理构造。
High Angle tabular cross bedding and low Angle wedge cross bedding are generally found on the cross section of the dunes.
矿脉呈中一陡倾斜柱板状产出，严格受断裂构造控制。
Orebearing veins are in the forms of inclined pillar or plate, medium to steep dipping and are controlled by fractures and faults.
矿脉呈中一陡倾斜柱板状产出，严格受断裂构造控制。
Orebearing veins are in the forms of inclined pillar or plate, medium to steep dipping and are controlled by fractures and faults.
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