摘要
新疆和静县位于新疆中部,在天山中段南麓,西北部为盆地,周边与乌鲁木齐市、库尔勒市等17个县市毗邻。和静县的矿产资源也很丰富,它的山地面积占地总面积的92.6%。红札铜金矿是一种位于博罗科努早古生代陆缘弧,是由于地质断裂构造活动强烈,使地壳侵入岩石层而发育形成的。矿床受到地层、火山岩、侵入岩、断裂等多种因素控制和影响,由岩浆作用形成并受断裂构造控制使其形成一种低温热液型的矿床。
Hejing county of xinjiang is located in the central part of xinjiang. It is located at the southern foot of the middle part of tianshan mountain. Hejing county is also rich in mineral resources, and its mountainous area covers 92.6% of the total area. Hongzha copper gold deposit is located in the early Paleozoic continental margin arc of bolokonu, which is formed due to the strong tectonic activity of geological faults and the intrusion of the crust into the lithosphere. The deposit is controlled and influenced by stratum, volcanic rock, intrusive rock, fault and other factors.
作者
赵雷
ZHAO Lei(The first regional geological survey brigade of the Bureau of Geology and mineral exploration and development,Urumchi 830013,China)
出处
《世界有色金属》
2018年第14期122-123,共2页
World Nonferrous Metals
关键词
新疆
红札铜金矿
地质特征
成矿规律
Xinjiang
red Zha copper gold deposit
geological characteristics
metallogenic regularity