闹牛山铜矿床火山机构控矿特征及次火山岩系列演化  

THE CHARACTERISTICS OF THE VOLCANIC MECHANISM- CONTROLLED ORES AND THE EVOLUTION OF SUB-VOLCANIC SERIES IN NAONIUSHAN COPPER DEPOSIT

作　　者：张百胜 

机构地区：[1]内蒙古有色地质勘查局108队,内蒙古赤峰024000

出　　处：《矿产与地质》2000年第5期299-302,共4页Mineral Resources and Geology

摘　　要：闹牛山铜矿床受火山机构控制 ,反映了成矿作用从供矿→运矿→集中→定位的全过程 ,次火山岩从基中性→中性→酸性方向演化 ,铜矿与次火山岩具有同空间、同时间 (或稍后 )、同源的特征。Naoniushan Copper deposit is controlled by volcanic mechanism, which reflect the whole process of the mineralization from ore-offering→transportation-concentration-emplacement and the subvolcanic rocks is evolved from basic→intermediate→acid rocks. The Copper ores show the characteristics of same space, and being contemporaneous and congeneric with sub-volcanic rocks. -

关 键 词：火山机构 次火山岩 成矿作用 铜矿床 控矿构造 岩浆 

分 类 号：P618.41[天文地球—矿床学] P588.13[天文地球—地质学]