摘要
金龙山—丘岭卡林型金矿床产于华北与扬子两地块会聚结合带的扩张海盆复杂岩相古地理沉积环境中。通过海底火山热液作用和生物活动的沉积成矿作用，形成成矿元素初始富集的矿源层。
The Jinlongshan-Qiuling carlin type gold deposit was formed under paleosedimentary environments with complicated lithofacies and in the spreading marine basin on the convergence between north China platform and Yangtze platform. The evolution of the deposit witnessed the formation of source bed with preliminary enrichment of ore-forming elements by marine volcanism and organism, and then mineralization by reformation.
出处
《地质与勘探》
CAS
CSCD
北大核心
1999年第5期20-23,共4页
Geology and Exploration
关键词
金矿床
成矿特征
卡林型金矿
秦岭
carlin gold deposit, mineralization, Jinlongshan-Qiuling, Qinling
