摘要
武夷山山口银多金属矿位于武夷成矿带光泽—宁化铜多金属成矿亚带东北部和浦城—宁德北西向钼多金属成矿带交汇处,矿体贮存于中生代焦坑组中,为沉积改造型矿床,主成矿期为晚三叠世。
The Shankou Silver polymetallic ore deposit located at the Wuyishan mineralization belt＇s gloss-The Ninghua copper polymetallic mineralizes northeast the Asian belt with Pucheng- North Ningde west to molybdenum polymetallic mineralization belt intersection point. The ore body tax has Mesozoic Era Jiao Kengzu in the stratum. For deposition transformation ore deposit. Controls the ore the north east to the fault zone is many phase of active products. The main metallogenic period is the late three pack of worlds. The Shankou area and peripheral further prospects the potential to be big.
出处
《福建地质》
2010年第2期96-100,共5页
Geology of Fujian
关键词
银多金属矿床
地质特征
沉积改造型
武夷山山口
Silver ore deposit, Geological feature, Deposition transformation, Wuyishan City
