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1.The folds and faults develop very much in the basin,and the former can be di- vided into 3 genetic types——regional compressive fold,local associated fold and drape-like fold,and the latter mainly shows 3 directions——near EW—NE,NW and NNE,in which the near EW—NE and NNE faults are well-developed relatively and control the distribution framework and sedimentary features of uplift and depression.
盆地褶皱、断裂构造十分发育,褶皱构造可划分为区域挤压型、局部伴生型和披盖型等三类,断裂构造主要可见近EW—NE向、NW向和NNE向三组,其中近EW—NE向和NNE向断裂比较发育,控制着盆地隆、坳分布格局和沉积特征。收藏指正
2.7.It is indicated the prospects for exploration are BeiDagang bueried-hill-drape-lik fold oil accumulation belt,Baidong Structure belt and Chengbei fault step oil accumulation belt,which directs the explorations of Neogene in Qikou depression.
7、指出了有利的勘探区带是北大港潜山—披覆背斜油气聚集带、白东构造带和埕北断阶式油气聚集带,为歧口凹陷上第三系的勘探明确了实施方向。收藏指正
3.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。收藏指正
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