摘要
新疆乌孙山地区 1号金矿是在对化探综合异常的查证过程中发现的。是伊什基里克山金、铜成矿带内发现的新类型金矿床。产于华力西中期花岗杂岩体的内外接触带附近的构造破碎带内 ,是构造蚀变岩型金矿床。矿化严格受断裂构造带和花岗杂岩体的控制。金矿体具规模较大、连续性良好、产状稳定及贫硫化物等特征。
The No.1 gold deposit, a new type gold deposit in Yishijike mountain Au Cu metallogenic belt in Wusun Mountain area, is discovered by checking geochemical prospecting anomaly. The mineralization zones(bodies) are strictly controlled by the faulted structural zones and the Variscan epoch′s granitic complex. The gold orebody has characteristics of large size, good continuty, stable occurrence and poor sulfide.
出处
《黄金地质》
2000年第1期22-26,共5页
Gold Geology
关键词
金矿床
地质勘探
地质特征
成矿带
新疆
Au Cu metallogenic zone
granitic complex
structural fracture altered rock
Xinjiang
