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贵州习水桑木场铅锌成矿带地质特征及找矿潜力
引用本文:刘金海.贵州习水桑木场铅锌成矿带地质特征及找矿潜力[J].贵州地质,2010,27(3):193-197.
作者姓名:刘金海
作者单位:贵州省地矿局102地质大队,贵州,遵义,563003
基金项目:致谢:在实验和成文过程中,得到中国科学院地球化学研究所周家喜博士的帮助和项目经费的资助,并提出了宝贵意见,在此表示衷心感谢.
摘    要:习水桑木场铅锌成矿带位于黔中隆起与四川盆地过渡部位桑木场背斜核部,通过对成矿带代表性矿床的地质特征和矿床成因等的研究,总结成矿带内铅锌矿床的成矿规律,并分析其成矿潜力,认为本区具有十分有利的成矿地质条件和利于赋矿的地层、构造空间,找矿潜力大,宜开展系统的地质工作,以实现地质找矿突破。

关 键 词:地质特征  找矿潜力  铅锌成矿带  桑木场背斜  贵州习水

Geologic Characters and Prospecting Potential of Sangmushang Lead-zinc Metallogenic Zone in Xishui,Guizhou
LIU Jin-hai.Geologic Characters and Prospecting Potential of Sangmushang Lead-zinc Metallogenic Zone in Xishui,Guizhou[J].Guizhou Geology,2010,27(3):193-197.
Authors:LIU Jin-hai
Institution:LIU Jin-hai (106 Geological Party,Guizhou Bureau of Geology and Mineral Exploration & Development,Zunyi 563003,Guizhou,China)
Abstract:Sangmuchang lead - zinc metallogenic zone situated in the anticlinal core of the transitional position of Central Guizhou uplift and Sichuan basin,by study the geologic character and deposit causation of representative deposit of the metallogenic zone,it summarized the regulation of lead - zinc deposit and analysis the potential,it' s thought that there has good mineral condition and layer,structural space,so the exploration potential is good and the systemic work for the breakthrough of exploration should be done.
Keywords:geologic character  prospecting potential  lead-zinc metallogenic zone  Sangmuchang anticline  Xishui  Guizhou
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