摘要
金青顶矿床地处胶东东部牟(平)—乳(山)金矿带内,将军石—曲河庄断裂为区内一级控矿构造,其成生经历了多期次的构造演化,由于构造—成矿期次的不同,产生了金的异型叠加成矿作用。
Jin-Qing-Ding Gold Deposit is situated in Mouping-Rushan gold
belt in the east part of Jiaodong Peninsula. Jiang-Junshi-Qu-He-Zhuang
fault belongs to the first order of ore-controlling structure in the gold belt, which experienced multiphase and multistage of tectonic evolution. Due to different phase and stage of tectogenesis and mineralization, the gold mineralization of variant superimposition produced.
出处
《黄金》
CAS
北大核心
1991年第8期7-11,共5页
Gold
关键词
金青顶矿床
金矿
叠加成矿
Jin-Qing-Ding Deposit
Jiang-Jun-Shi-Qu-He-Zhuang fault
tectogenesis and phase of mineralizationi superimposed mineralization
variant superimposition
