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河南桐柏老洞坡银成矿带地球化学特征及找矿标志
引用本文:简庆伟.河南桐柏老洞坡银成矿带地球化学特征及找矿标志[J].四川地质学报,2014(2):267-271.
作者姓名:简庆伟
作者单位:河南省地质矿产勘查开发局第三地质矿产调查院,河南信阳464000
摘    要:老洞坡银矿床位于围山城成矿带东延部,出露地层由下古生界大栗树组(Pz1d)和上古生界歪头山组(Pt3w)组成。老洞坡银矿体的发现显示歪头山组地层上、中、下三部均为含矿层,银矿体受朱庄背斜,歪头山组下部第五岩性段和构造控制。查明该矿床的原、次生地球化学异常特征,将老洞坡银矿床与破山、银洞坡银矿床的地质地球化学特征进行对比研究,在指导找矿上具实际意义。

关 键 词:银矿床  地球化学  含矿层  桐柏老洞坡

Geochemical Characteristics and Ore Criteria for the Laodongpo Ag Deposit in Tongbai,Henan
JIAN Qing-wei.Geochemical Characteristics and Ore Criteria for the Laodongpo Ag Deposit in Tongbai,Henan[J].Acta Geologica Sichuan,2014(2):267-271.
Authors:JIAN Qing-wei
Institution:JIAN Qing-wei (No.3 Institute of Geological Survey, Department of Geology and Mineral Resources of Henan Province, Xinyang, Henan 464000)
Abstract:The Laodongpo Ag deposit in the Weishancheng ore belt is confined to the Upper Paleozoic Waitoushan Formation(Pt3w). The orebodies are controlled by the Zhuzhuang anticline and lithologic character. Preliminary and secondary geochemical anomalies for the deposit may be correlated with those for the Poshan and Yindongpo deposits.
Keywords:Ag deposit  geochemistry  ore-bearing formation  Laodongpo  Tongbai
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