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北山地区总体属塔里木板块东北边缘 ,矿产丰富。北山中带属塔里木古大陆边缘向陆一方的伸展系统。红柳河弧后扩张盆地、黑山—花牛山及营毛沱—白湖一带属该伸展体制下的裂谷构造单元。本区基性、超基性杂岩共分两大类 ,一类是裂谷作用早期形成的基性、超基性杂岩 ,另一类是裂谷作用鼎盛时期抑或是弧后海盆 (洋盆 )阶段形成的基性—超基性杂岩 ,也称之蛇绿杂岩。前者除黑山岩体和柳园岩体之外 ,还有大山头、庙庙井复式岩体②、黑山北岩体⑤、马鬃山复式杂岩体⑨及营毛沱北岩体④ ;后者除红柳河、玉石山蛇绿杂岩①及牛圈子蛇绿杂岩⑧之外 ,还有独红山岩体③、锡林柯博岩体⑥、双井岩体⑦等。前者形成于中元古代 ,后者形成于早古生代 ,镍铜成矿系统与前者关系密切。
Beishan area is generally the northeastern edge of the Tarim plate, rich in minerals. Beishan belonged to Tarim ancient continent edge of the extension of the system to the land. The Hongliuhe arc-back dilation basin, Montenegro-Huynone Mountain and Yingmintuo-Baihu area belong to rift structural units under the extensional system. The basic and ultramafic complexes in this area are divided into two broad categories, one is the basic and ultrabasic complex formed early in the rifting process, and the other is whether the rifting or heliotrophic basin Basin) formed during the basic - ultrabasic complex, also known as ophiolite. The former includes Montenegro rock mass and Liuyuan rock mass, as well as Dashantou, Miaomiaojing complex rock ②, Montenegro rock mass ⑤, Mazongshan complex ⑨ and Yingmaotuo north rock ④; In addition to the Hongliuhe, Jade Mountain Yuken complex ① and cattle circle snake green ⑧ ⑧, there are Dulongshan ③, Xilin Ke Bo rock ⑥, double rock ⑦ and so on. The former is formed in the Mesoproterozoic, the latter formed in the early Paleozoic, nickel-copper metallogenic system and the former are closely related.