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39Ar-40Ar dating of Gejiu tin deposit and its origin, Yunnan, China

机译:39AR-40AR约会Gejiu锡矿床及其起源,云南,云南

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Gejiu tin ore deposit is a famous tin-polymetallic deposit throughout the world because of its old mining history and its enormous metal reserves.In addition to tin metal,there are copper,lead,zinc,silver,iron.sulphur,tungsten,bismuth,indium and rare earth elements.It was believed that there mainly are skarn-type tin deposit,stratiform tin deposit and basalt-type copper deposit in Gejiu tin poly-metallic orefield.The stratiform tin deposit are distributed in Lutangba,Malage and Huangmaoshan,which are hosted by carbonate rocks of Gejiu formation in Middle Triassic Series.In this paper,40Ar-39Ar dating of cassiterite from the sratiform tin deposit in Lutangba yields plateau age of 202.18 + 2.35 Ma and isochron age of 206.81 + 3.23 Ma respectively.The ages are obviously older than those of the ore of the skarn type deposit of the Yanshanian epoch.The mineralization is the seabed exhalative hydrothermal sedimentary mineralization of the Indosinia epoch.
机译:Gejiu锡矿床是世界各地着名的锡多金属矿床,因为其旧的采矿历史及其巨大的金属储备。除锡金属外,还有铜,铅,锌,银,铁。森林,钨,铋,据信铟和稀土元素。主要是矽卡布锡锡多金属壁壁板上的矽卡岩型锡矿床,层状锡矿床和玄武岩型铜矿矿物。岩石型锡矿床分布在Lutangba,Malage和Huangmaoshan中由中间三叠系系列的Gejiu组碳酸盐岩载体。本文,从Lutangba的Sriford TiN矿床进行40AR-39ar约会,产量分别为202.18 + 2.35 mA和同上的等值分别为206.81 + 3.23 mA。显然比燕山纪元的矽卡岩型矿床矿床较大。矿化是Indosinia时期的海底呼气水热沉积矿化。

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