首页 | 本学科首页   官方微博 | 高级检索  
     检索      

福建何宝山金矿控矿构造地球化学特征及其剥蚀程度初探
引用本文:林仟同,魏孝秋.福建何宝山金矿控矿构造地球化学特征及其剥蚀程度初探[J].福建地质,1994,13(1):1-10.
作者姓名:林仟同  魏孝秋
作者单位:闽北地质大队
摘    要:本文以何宝山矿段为典型实例,较系统地论述了矿区主要控矿构造地球化学特征,探讨了矿区原生晕指示元素分带序列和金矿化剥蚀程度。认为矿区主矿带何宝山矿段Ⅱ号矿化带南北两段产状及剥蚀程度的差异,系受东百向张扭性断裂(F5)成矿后活动影响所致。

关 键 词:控矿构造  金矿床  地球化学

On the Geochemical Characteristics of Ore-controlling Structures and Denudation of the Hebaoshan Gold Ores in Fujian Province
Lin Qiantong,Wei Xiaoqiu,Gong Ping.On the Geochemical Characteristics of Ore-controlling Structures and Denudation of the Hebaoshan Gold Ores in Fujian Province[J].Geology of Fujian,1994,13(1):1-10.
Authors:Lin Qiantong  Wei Xiaoqiu  Gong Ping
Abstract:This paper focuses on the geochemical characteristics of major ore-controlling structures, zoning sequence of indicator elements from the primary halo and denudation in the Hebaoshan Gold Ores. The Hebaoshan Gold Ores is situated at the intersection point of the Chongan-Shicheng Structural Belt and Jianning-Jianou Structural Belt in Fujian Province. Take the Hebaoshan ore block as an example, which is the major ore belt of the Hebaoshan Gold Ores. It is concluded that the difference of occurrence and denudation between the southern and northern ore blocks in the No. 2 mineralizational belt of the Hebaoshan ore block results from the tensomshear fault of the EW trend.
Keywords:Fujian Province  geochemical characteristics  Hebaoshan Gold Ores  indicator Elements  ore-controlling structure  primary halo  
本文献已被 CNKI 维普 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号