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Geochemical Characteristics of Rare Earth Elements in Gejiu Tin Polymetallic Deposits, Yunnan Province, China

机译:云南省旧旧多金属矿床中稀土元素的地球化学特征

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In order to get a better understanding- of metallogeny, the geochemical characteristics of REE and trace element for Gejiu tin polymetallic deposits were studied by comparing concentrations of REE and trace elements in different type ores and rocks, including skarn-type ore, bedded-type ore, vein-type ore, altered granite, country rocks. Results of this study indicated that the metallogenic matters for different type ores in the study area might be derived from the same origin source, which may be mainly related to granitic activities . Furthermore, there are some differences in concentrations of REE in different ores due to their different depositional mechanism during that time. LREE concentrations were enriched relatively in the vein-type ores and the bedded-type ores with relatively low total REE concentrations, whereas total REE concentrations were higher in the skarn-type ores with LREE and HREE concentrations in wide variation ranges.
机译:为了更好地了解成矿作用,通过比较不同类型矿石和岩石(包括矽卡岩型,层状型)中稀土元素和微量元素的含量,研究了旧旧锡多金属矿床的稀土元素和微量元素的地球化学特征。矿石,脉状矿石,变质花岗岩,乡村岩石。研究结果表明,研究区不同类型矿石的成矿物质可能来源于同一来源,可能主要与花岗岩活动有关。此外,由于在此期间不同的沉积机理,不同矿石中的REE浓度也存在一些差异。总REE浓度相对较低的静脉型和层状矿石中,LREE浓度相对富集,而矽卡恩型矿石中的LREE和HREE浓度范围较宽,总REE浓度较高。

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