摘要
在总结清白山铅锌矿矿床地质特征、控矿因素的基础上,通过与MVT型矿床典型特征对比,认为其成因类型为MVT型。通过总结控矿因素,讨论了成矿时代,初步建立成矿模型,认为矿床成型分为含矿流体沉淀的主成矿期、构造改造期、岩浆改造期3个阶段。
Based on the summary of the geological characteristics and ore-controlling factors of the Qingbaishan lead- zinc deposit,the authors consider that the genetic type is MVT type by comparing with the typical characteristics of the MVT deposit.By summarizing the ore-controlling factors,the metallogenic age is discussed.The metallogenic model was established.It is believed that the formation of the deposit is divided into three stages:main ore-forming period,tectonic transformation period and magma transformation period.
作者
夏天
Xia Tian(Xinjiang geological suvey academy,Urumqi,Xinjiang,830000,China)
出处
《新疆地质》
CAS
CSCD
北大核心
2019年第3期309-312,共4页
Xinjiang Geology
关键词
地质特征
MVT型铅锌矿床
成矿时代
成矿模型
Geological characteristics
MVT-type lead-zinc deposit
Metallogenic age
Metallogenic model
