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河南马超营—独树一带银铅锌成矿地质条件及找矿前景
引用本文:燕长海,刘国印,宋 锋,张正伟.河南马超营—独树一带银铅锌成矿地质条件及找矿前景[J].中国地质,2002,29(3):305-310.
作者姓名:燕长海  刘国印  宋 锋  张正伟
作者单位:1. 中国地质大学,北京,100083;河南省地质调查院,河南,郑州,450007
2. 郑州大学商学院,河南,郑州,450052
基金项目:国土资源大调查项目(199910200227)和国家自然科学基金项目(40072003)联合资助.
摘    要:马超营-独树一带位于华北陆块南缘,为一元古宙-古生代裂陷槽。官道口群、栾川群和陶湾群为滨海、浅海、陆棚相陆缘碎屑-碳酸盐岩沉积建造,强烈的浅源火山喷(气)发活动,形成多层硅质条带(团块)、硅质岩以及含Ag、Pb、Zn矿化的层状夕卡岩带。该带是比较典型的地球化学急变带与地球物理梯度带交叉区,壳、幔富含Mo、Pb、Zn、Au元素。基于该带银铅锌金矿成矿地质条件,推断具有良好的找矿前景。

关 键 词:银铅锌金矿床  形成条件  找矿前景  河南  火山喷发活动  成矿地质条件
文章编号:1000-3657(2002)03-0305-06

Ore-forming geological conditions and ore prospects of silver-lead-zinc-gold deposits in the Maochaoying-Dushu area, Henan
YAN Chang-hai ,LIU Guo-yin ,SONG Feng ,ZHANG Zheng-wei.Ore-forming geological conditions and ore prospects of silver-lead-zinc-gold deposits in the Maochaoying-Dushu area, Henan[J].Chinese Geology,2002,29(3):305-310.
Authors:YAN Chang-hai    LIU Guo-yin    SONG Feng    ZHANG Zheng-wei
Institution:YAN Chang-hai 1,2,LIU Guo-yin 1,2,SONG Feng 1,2,ZHANG Zheng-wei 3
Abstract:The Maochaoying-Dushu area on the southern margin of the North C hina block is a Protero-zoic-Paleozoic aulacogen,where there occur littoral ,neritic and shelf continental-margin clastic-carbonate formations of the G uandaokou Group,Luanchuan Group and Taowan Group.Strong shallow-source vol-c anic eruption(exhalation)gave rise to multi-layer chert bands(nodules),sil iceous rocks and silver-lead-zinc mineralization-bearing layered skarn in th e area.This area is a relatively typical district where a geo-chemical abrupt change zone and a geophysical gradient zone intersect.The earth's mantle and crust be-neath the area are enriched in Mo ,Pb,Zn and Au.From the ore-form ing geological conditions of sil-ver-lead-zinc-gold deposits,it is inferr ed that the area has good ore prospects.
Keywords:silver-lead-zinc-gold de posit:ore-forming conditions  ore prospects  Maochaoying-Dushu:Henan Provin ce
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