福建省大田县建爱矿区铁多金属矿地质特征及成因浅析  

Geological characteristics and genesis of iron polymetallic ore in Jianai mining area, Datian County,Fujian Province

作　　者：刘少云 LIU Shao-yun(The Western Geological Party of Fujian,Sanming 365000,China)

机构地区：[1]福建省闽西地质大队,福建三明365000

出　　处：《世界有色金属》2021年第21期75-76,共2页World Nonferrous Metals

摘　　要：结合本区从打开储矿通道(F_(0)、F_(0)′)、热液成矿、再接受后期构造破坏的整个过程,形成一套由船山组、栖霞组灰岩层位和滑脱构造双重控制的层控(矽卡岩型)铁硫多金属矿床。Combined with the whole process of opening ore storage channels(F_(0),F_(0)'),hydrothermal mineralization and later structural damage in this area,a set of stratabound(skarn type)iron sulfur polymetallic deposits controlled by the limestone horizon and detachment structure of Chuanshan formation and Qixia Formation are formed.

关 键 词：推覆构造 铁帽 断层泥 矽卡岩化 层控矽卡岩型 

分 类 号：P618.2[天文地球—矿床学]