甘肃夏河地区加木龙沟金矿矿床地质特征分析

Analysis of Geological Characteristics of the Gold Deposits in Jiamulonggou,Gansu Province

加木龙沟金矿床位于西秦岭造山带西段之西秦岭褶皱带的南秦岭被动陆缘带,属于夏河—合作金成矿带的重要组成部分,区内构造—岩浆活动强烈,成矿地质背景条件优越.本文在分析矿床地质背景的基础上总结了矿床地质特征,为进一步开展矿床成因以及成矿规律研究提供参考.

The Kamulonggou gold deposit is located in the South Qinling passive land margin belt of the West Qinling fold belt in the western section of the West Qinling Mountain Belt,which belongs to the important part of the Xiahe-Cooperative Gold-forming Mineral Belt,and the tectonic-magma activity in the region is strong,and the geological background conditions of mineralization are superior.Based on the analysis of the geological background of the deposit,this paper summarizes the geological characteristics of the deposit,and provides reference for further research on the causes of mineral deposits and the law of mineralization.