By studying,The JinChangGou Cu-Mo Deposits is a type of breccia which relate to granodiorite who had intruded superficial.

• 研究认为金场沟区铜钼矿是与超浅成花岗闪长岩体侵入有关的角砾岩型矿床,受北东和北西向断裂构造控制。