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The Pb-Zn deposits and mineralization during Cambrian in Chongqing area of Yangtze Platform, China

机译:中国长江平台重庆地区寒武纪的PB-ZN沉积和矿化

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This paper presented the Pb-Zn deposits characteristics in southeast Chongqing. The Pb-Zn deposits occurred in Lower-Middle strata with develop the dolomites, limestones as ore-bearing host-rocks. They are veined, stratifed, stratoid, and lenticular in shape and locally pinch and swell with dominant ore minerals of sphalerite, galena, and pyrite . the Pb-Zn ore deposits grade changed from 0.32% to 7.06% for Pb and 4.21% to 14.29% for Zn. The Gaodongzi orebody has highest concentrations of Pb with 7.06% record and Zn with 14.29% record. The tectonic setting, ore-host rocks, wall-rock alternation, and mineral composition will control the Pb-Zn deposits distribution in Chongqing area.
机译:本文介绍了重庆东南部的PB-Zn沉积特征。 PB-Zn沉积物发生在低中间地层,与含有矿石宿主岩石的白云岩,石灰石发生。它们是脉冲,分层,色度和晶状体形状,局部夹住,含有斯普利纳,高利纳和黄铁矿的优势矿石矿物质。 PB-Zn Ore沉积级别从Pb的0.32%变为7.06%,Zn的4.21%至14.29%。高孔矿矿体具有最高浓度的PB,记录7.06%,ZN记录14.29%。构造,矿石岩石,壁岩交替和矿物组合物将控制重庆地区的PB-Zn沉积物分布。

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