王常微,张克信,何卫红,杨忠琴,杨廷禄,胡从亮,张扬,邓毅,于志松.贵州威宁鱼坝稀土含矿岩系的锆石U-Pb年龄[J].贵州地质,2020,37(1):14-23
贵州威宁鱼坝稀土含矿岩系的锆石U-Pb年龄
Zircon U-Pb Age of Yuba Rare Earth-bearing Rock Series in Weining, Guizhou
投稿时间:2019-09-17  
DOI:
中文关键词:  锆石U-Pb年龄  稀土矿  含矿岩系  威宁鱼坝  黔西北
英文关键词:Zircon U-Pb age  Rare earth deposit  Ore-bearing rock series  Yuba Weining  Northwest Guizhou
基金项目:本文为贵州省地质矿产勘查开发局地质科研项目“黔西北晚二叠世稀土成矿作用与形成机理研究”(黔地矿科合201509)成果。贵州省科技计划项目:贵州省地质调查院院士工作站(编号:黔科合平台人才[2018]5626)、贵州省地质物探开发应用工程技术研究中心(编号:黔科合[2016]平台人才5401)。
作者单位E-mail
王常微 中国地质大学武汉地质调查研究院武汉430074
贵州省地质调查院贵阳550081 
wchw91831@sina.com 
张克信 中国地质大学武汉地质调查研究院武汉430074  
何卫红 中国地质大学武汉地质调查研究院武汉430074  
杨忠琴 贵州省地质调查院贵阳550081  
杨廷禄 中国地质大学武汉地质调查研究院武汉430074  
胡从亮 贵州省地质调查院贵阳550081  
张扬 中国地质大学北京北京100083  
邓毅 贵州省地质调查院贵阳550081  
于志松 中国地质大学武汉地质调查研究院武汉430074  
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中文摘要:
      黔西北地区晚二叠世稀土矿产于峨眉山玄武岩与上伏宣威组假整合面附近,在威宁地区稀土矿分为上、下两层,下含矿层为浅灰白色高岭石粘土岩,上含矿层为浅灰色高岭石粘土岩与铝质高岭石粘土岩,含矿岩系厚度在区域上变化较大,在威宁鱼坝剖面含矿岩系完整且厚度较大。在含矿岩系底部凝灰质粘土岩中取样测得锆石U-Pb平均年龄为25411 Ma±098 Ma,含矿岩系顶部熔结凝灰岩锆石U-Pb年龄为2520 Ma±082 Ma(谐和年龄)和2519 Ma±186 Ma(平均年龄)。证实黔西北晚二叠世稀土含矿岩系下矿层产于峨眉山玄武岩第三段上部、上矿层产于宣威组下段,整个稀土含矿岩系形成时间约为2 Ma。
英文摘要:
      In the northwest Guizhou, the rare earth deposit in late Permian is found near the disconformity surface of Emeishan basalt and upper Xuanwei formation, the rare earth deposit in Weining area is divided into upper and lower two layers, the lower layer is light gray white Kaolinite clay rock, the upper layer is light gray kaolinite clay rock and aluminous kaolinite clay rock, the thickness of the ore-bearing rock series has big change in this area. The ore-beaing rock series is complete and the thickness is big in the profile of Yuba, Weining. It taken samples in tuffaceous clay rock which in the bottom of ore-bearing rock series, the tested average zircon U-Pb age is 254.11 Ma±0.98 Ma, the zircon U-Pb age of welded tuff in the top ore-bearing rock series is 252.0 Ma±0.82 Ma(concordant age)和251.9 Ma±1.86 Ma(average age). it’s proved that the lower layer of rare earth ore-bearing rock series of late Permian in northwest Guizhou occur in the upper 3rd section of Emeishan basalt, the upper layer occur in the lower Xuanwei formation, the formation age of the whole rare earth ore-bearing rock series is about 2 Ma,
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