区内线状褶皱及纵向断裂发育,双王金矿处于区域西坝-松坪复式向斜的北东翼。 矿区南侧出露有狮子岭中酸性岩体,展布方向与区域构造线相一致,岩体长约30km,宽2~8km。其主体为石英二长闪长岩,晚期为二长花岗岩,均属印支期产物。矿区内发育有闪斜煌斑岩及少量花岗斑岩、石英钠长斑岩等脉岩,呈北东向延长,均横切金矿体。 The development zone inside folds and longitudinal fracture, Shuangwang gold deposit in north east wing area - the Song Ping Xiba synclinorium.
矿区南侧出露有狮子岭中酸性岩体,展布方向与区域构造线相一致,岩体长约30km,宽2~8km。其主体为石英二长闪长岩,晚期为二长花岗岩,均属印支期产物。矿区内发育有闪斜煌斑岩及少量花岗斑岩、石英钠长斑岩等脉岩,呈北东向延长,均横切金矿体。
In the south of the mining area, there is an acidic rock mass in the middle of the south of the mountain, which is consistent with the regional tectonic line. The rock mass is about 30km and the width is 2 to 8km. The main body of quartz two long Shan Changyan, two in late Indosinian granite, are the product of. Within the mining area development flash oblique lamprophyre and a small amount of granite porphyry and quartz albite porphyry dykes, a North East to extend, crosscutting gold ore bodies.
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