金中国.黔西北垭都- 蟒硐断裂带铅锌成矿地
质特征及找矿潜力分析[J].地质与勘探,2009,45(2):20-26 |
黔西北垭都- 蟒硐断裂带铅锌成矿地
质特征及找矿潜力分析 |
Lead - ZincM inera liza tion Character istics and Explora tion Poten tia lof the Yadu - Mangdong Fault Belt in Northwestern Gu izhou |
投稿时间:2008-07-07 修订日期:2008-10-27 |
DOI: |
中文关键词: 铅锌矿床 地质特征 垭都- 蟒硐成矿带 黔西北 |
英文关键词: lead - zinc deposit geology metallogeny YaDu - MangTongmetallogenic belt, nouthwest Guizhou |
基金项目:国土资源大调查项目(项目编号200410200019)和资源补偿费项目(任务书编号200501003)联合资助。 |
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中文摘要: |
[摘要]文章论述了垭都- 蟒硐铅锌成矿带成矿地质条件,断层控岩、控矿特点。从区域地质地球
化学背景、典型矿床产出特征,总结了垭都- 蟒硐断裂带铅锌成矿规律。找矿实践证明,垭都- 蟒硐断
裂带内铅锌矿体主要呈陡脉状产出,旁侧次级断裂带中则呈层状产出;断层活动强度与铅锌矿化常成正
相关关系;成矿地质条件、物化探异常特点、铅锌矿化富集特征显示,垭都、筲箕湾、羊角厂矿区深部及外
围具备寻找大型铅锌矿床的潜力。 |
英文摘要: |
Abstract:This paper discussed the geology and metallogeny of lead - zinc mineralization in the YaDu - - MangDongmetallogenic belt. Based on re2
gional geological and geochemical background and characters of known typ ical deposits and occurrences in the region, the lead - zinc mineralization rules
are summarized. The exp loration in the region shows that faults in the YaDu - - MangDong lead - zinc mineralization belt are the main ore - controlling
structures, ore - bodies in major fractures are mainly occurred as steep ly dipp ing veins, whereas and ore - bodies in nearby subsidiary fractures are mainly
stratiform. The fault activity strength is positively related with the lead - zincmineralization intensity. The geology, geophysical and geochemical anomalies
and mineralization concentration rules all suggested that there are exp loration potentials for discovering large lead - zinc deposits in the deeper section of
the YaDu, ShaoJ iWan and YangJueChangmining areas and also peripheral areas of the mines |
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