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澜沧老厂红土型银矿床成矿条件及找矿标志
引用本文:陈百友,王增润,张映旭,陈伟.澜沧老厂红土型银矿床成矿条件及找矿标志[J].中南大学学报(自然科学版),2000,31(3):195-198.
作者姓名:陈百友  王增润  张映旭  陈伟
作者单位:中南工业大学资源环境与建筑工程学院!湖南长沙410083(陈百友,王增润),西南有色地质勘查院!云南昆明650216(张映旭,陈伟)
基金项目:国家“九五”科技攻关计划资助项目! ( 96 914 0 3 0 5 0 1)
摘    要:老厂红土型银矿床含银矿源体为中上石炭统碳酸盐岩 .通过研究该矿床成矿条件 ,认为含银矿源体的形成与大陆边缘裂谷构造和中晚石炭世沉积喷流作用密切相关 ,并与早石炭世火山作用有间接联系 ;银的次生富集条件是温暖潮湿的古气候、相对平缓的古地貌、碳酸盐岩岩性和中上石炭统地层层位 .最后提出了老厂式红土型银矿床的找矿标志

关 键 词:红土型银矿床  成矿条件  找矿标志  老厂

Metallogenic conditions and prospecting criteria of Laochang lateritic silver deposit, Lanchang
CHEN Bai you ,WANG Zeng run ,ZHANG Ying xu ,CHEN Wei.Metallogenic conditions and prospecting criteria of Laochang lateritic silver deposit, Lanchang[J].Journal of Central South University:Science and Technology,2000,31(3):195-198.
Authors:CHEN Bai you  WANG Zeng run  ZHANG Ying xu  CHEN Wei
Institution:CHEN Bai you 1,WANG Zeng run 1,ZHANG Ying xu 2,CHEN Wei 2
Abstract:The silver bearing source unit of the Laochang lateritic silver deposit is carbonate rock of middle and upper Carboniferous. This paper deals with the metallogenic conditions of the deposit. It is suggested that the formation of the silver bearing source unit has a great deal to do with continental marginal rift structure and sedimentary exhalation of middle and late Carboniferous and has some indirect relations with early Carboniferous volcanicity. The conditions of silver secondary enrichment are warm and humid paleo climate, relatively gentle paleo topography, lithololgy of carbonate rock and stratigraphic horizon of middle and upper Carboniferous. The prospecting criteria for Laochang type lateritic silver deposit was put forward in the end.
Keywords:lateritic silver deposit  metallogenic conditions  prospecting criteria  Laochang
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