福建省永定区樟坑铁铜矿地质特征及成因探讨

Geological Characteristics and Genesis of Zhangkeng Iron and Copper Deposit in Yongding District,Fujian Province

福建省永定县樟坑-张岩下铁铜矿区位于马坑铁矿田的南西侧,是铁多金属成矿的有利地区,整合区位于上古生代闽西南拗陷带的大田-龙岩拗陷内,属龙岩山字型脊柱东侧与前弧内侧的汇合部,王庄-樟坑推覆构造体南部,是成矿的主要因素。

Pick to yongding district of fujian province under the camphor pit-metcalf jv iron and copper mining area located in the south west side horse iron mine field,are favorable for fe polymetallic metallogenic region,consolidation area in the field of upper Paleozoic MinXiNa geotectogene-in longyan depression,hill type spine on the east side with the former belongs to the convergence of the inside of the arc,south wangzhuang-camphor pit nappe structure,is the main factor of mineralization.