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浅论湖南省银异常分布特征和找矿方向
引用本文:张子清.浅论湖南省银异常分布特征和找矿方向[J].湖南地质,1991,10(3):229-234.
作者姓名:张子清
作者单位:湖南省地质矿产局物探队 邵阳422002
摘    要:湖南省银矿床银主要来源于岩浆源,已发现的银矿床主要有三类:矽卡岩型银铅锌矿床,脉状热液型银铜铅锌矿床,斑岩型银多金属矿床。银矿的分布受大地构造的控制:属扬子准地台上扬子台褶带的湘西北区无岩浆侵入活动,无银矿点分布,也末发现银异常;属扬子准地台江南台隆的雪峰古陆过渡区,银异常密集分布,强度中等,系沉积型含银的钒磷矿分布区,尚未发现工业银矿床,属华南褶皱系赣湘桂粵褶皱带的湘中、湘南、湘东区,银异常呈点状分布,强度大,是主要岩浆源型银矿分布区,是银矿找矿的重点地区。

关 键 词:银矿  地球化学异常  勘探  湖南  矿床

ELEMENTARY DISCUSSION ON THE DISTRIBUTION OF SILVER ANOMALIES IN HUNAN PROVINCE AND DIRECTION OF PROSPECTING
Zhang Ziqing.ELEMENTARY DISCUSSION ON THE DISTRIBUTION OF SILVER ANOMALIES IN HUNAN PROVINCE AND DIRECTION OF PROSPECTING[J].Hunan Geology,1991,10(3):229-234.
Authors:Zhang Ziqing
Institution:Geophysical Exploration Team of Hunan Bureau of Geology and Mineral Resources
Abstract:The silver of the silver deposits in Human province is mainly derived from magma sources. The silver deposits proved can be grouped into three types: Skarn type silver-lead-zinc deposit, Hydrotermal vein type silver-copper-lead-zinc one and porphyry type silver-polymetallic one. The distribution of sliver deposits is controlled by the geotectonic setting: In the Northwestern Hunan, which is a part of Upper Yangtze platformal fold belt of Yangtze sub-platform, without magmatic intrusion, there is no occurrence of silver deposit, even silver anomalies; The Xuefeng old landmass transition region, which is a part of Jiangnan platform uprise of Yangtze sub-platform, yields silver-bearing sedimentary type vanadium-phosphorus mineralizations, with condensed silver anomalies, medium in intensity, but no economic silver deposit has been found yet; while the Central, Southern and Eastern parts of Hunan, which belong to Gan-Xiang-Gui-Yue fold belt of South China told system, are the main magma-derived silver deposit-distributing region, with high-intensity silver anomalies occurring dotted, which is considered to be the key prospect for silver deposits.
Keywords:Silver  Geochemical exploration  Direction of prospecting  Geochemical anomaly
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