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福建柘荣马坑银矿地质特征及找矿方向
引用本文:陈龙照,黄仕浩,苏树辉.福建柘荣马坑银矿地质特征及找矿方向[J].地质找矿论丛,2012,27(1):55-59.
作者姓名:陈龙照  黄仕浩  苏树辉
作者单位:中国冶金地质总局第二地质勘查院,福建莆田,351111
摘    要:福建省柘荣县马坑银矿产于上侏罗统-下白垩统陆相酸性火山岩中,矿体严格受断裂(F1,F2)及其派生裂隙的控制。矿床发育绢云母化、硅化、黄铁矿化、黄铁绢英岩化、青磐岩化等中低温热液蚀变,矿体地表呈密集细脉状,深部为简单板状、透镜状。矿石矿物以自然银为主,次为辉银矿,含少量方铅矿、闪锌矿等。矿石工业类型为硫化矿,矿床成因为受断裂构造控制的中低温浅成火山热液充填交代型银矿床。

关 键 词:马坑银矿  地质特征  找矿方向  福建省
收稿时间:2010/12/22 0:00:00
修稿时间:2011/4/8 0:00:00

Geological characteristics of Makeng Ag deposit and the ore-searching directions in the mining district
CHEN Long-zhao , HUANG Shi-hao , SU Shu-hui.Geological characteristics of Makeng Ag deposit and the ore-searching directions in the mining district[J].Contributions to Geology and Mineral Resources Research,2012,27(1):55-59.
Authors:CHEN Long-zhao  HUANG Shi-hao  SU Shu-hui
Institution:(The 2nd Geological Exploration Institute of China Metallurgical Geological Bureau, Putian 351111,Fujian,China)
Abstract:Makeng Ag deposit in Zherong county,Fujian province occurs in continental acid volcanics of Upper Jurassic-Lower Cretaceous series and is controlled strictly by fault F1,F2 and the derivative fractures.In the deposit are develped medium-epithermal alterations,such as serisitization,silicification,pyritization,phyllic alteration and propyllitization.At surface it is in closely spaced small veins and simple tabular body and lens to depth.Native silver is the main ore mineral then argenite and a few galena and sphalerite.Industrially the ore is of sulfidation type and genetically the deposit is the fracture-controlled medium-epithermal fluid filling and replacement silver deposit..
Keywords:Makeng Ag deposit  geological characteristics  the ore-searcing dirction  Fujian province
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