摘要
银洞山铅锌矿区位于华北地台南缘以南的活动带,属阿森特—加里东地槽型陆缘海沉积变质相,区内岩浆活动频繁,构造广泛发育,是成矿的有利地带。通过对该区矿床地质特征的总结,指出本区金属矿床具有多成因叠加特点,属与一定的地层岩性组合有关的热液矿床,对指导该矿区下一步地质勘查及找矿,扩大资源具有积极的作用。
The Yindongshan Pb-Zn deposit is located at the active belt northwards to southern edge of North China Platform,which belong to Asente-Caledonian continental sources marine sedimentary metamorphic phase of geosyncline type.With active magmatic movements and broad development of structure,the studying area is a favorable area for mineralization.According to the conclusion of the geological characteristics of the deposit in this area,the study has pointed out that the metallic deposits in this mining area are...
出处
《矿产与地质》
2009年第2期114-117,共4页
Mineral Resources and Geology
关键词
铅锌矿床
多成因叠加
地质特征
矿床类型
银洞山
南召
河南
Pb-Zn deposit
superposition with multiple genesis
geological characteristics
types of deposits
Yindongshan
Nanzhao
Henan