摘要
北东向深大断裂成矿前生成,控制岩浆岩侵入及成矿带展布,多期次构造、岩浆活动,提供成矿物质及其活化热源。矿床具典型的水平垂向分布规律。应用构造地球化学方法找矿效果显著。
The NE macrofault is formed before the metallogenesis,which has controlled the intrusion of magmatic rock and the distribution of metallogenetic zone.The multiphasic structure-magmatic activities provide the metallogenetic material and the heat source of activization.The ore deposit has the typical horizontal and vertical distribution rule.The application of structure-geochemical prospecting method has the clear results.
出处
《云南地质》
2013年第1期56-59,共4页
Yunnan Geology
关键词
铜多金属矿
南北中各不相同
构造控矿
成矿规律明显
桂东大瑶山北侧
Cu Multimetallic Deposit
Different One Another in N
Mid
S
Ore Control of Structure
Metallogenetic Rule Clear
N Dayaoshan
E Guangxi
