论文部分内容阅读
以构造地质及构造地球化学等研究为依据，重新厘定了水沟—时金河断裂的规模，弄清了它的引张压扭张扭的构造性质，探讨了断裂形成时代、演化历史及其对岩浆作用和成矿作用的控制规律。认为该断裂具有导容矿双重性。导矿作用发生在断裂的开放构造环境及相关部位，并在其两侧形成石英脉金矿床。容矿作用发生在断裂的封闭构造环境及相关部位，在断裂内形成蚀变岩型金矿床。实现了找矿勘探方向由派生断裂向主干断裂的战略转移，为扩大金矿资源开辟了新途径。
Based on the study of tectonic geology and tectono-geochemistry, the scale of Shuigou-Shijinhe fault was redetermined and the tectonic properties of its tensile-torsional-torsional torsional deformation were discussed. The formation age and evolution history of the fault And its control law on magmatism and mineralization. It is considered that the fracture has the duality of conducting ore. The ore-bearing action takes place in the open tectonic environment and related parts of the fault, and forms quartz vein gold deposits on both sides. The ore-hosting effect occurs in the closed fault tectonic environment and related parts, forming altered rock type gold deposits within the fault. It has realized the strategic shift of the prospecting direction from the derived fault to the main fault and opened up a new way for expanding the gold resources.