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Helium-argon isotopic tracing for the Pb-Zn-Ag polymetallic ore deposits in the central-south segment of the Da Hinggan Ling Range

机译:大兴安岭岭中南段铅-锌-银多金属矿床的氦-氩同位素示踪

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In recent years big strides have been made in the exploration of ores in the central-south segment of the Da Hinggan Ling Range, though some debates still exist on the metallogenesis and sources of ore-forming materials.Pyrite and other sulfides in direct relation to the Pb-Zn-Ag ore deposits were chosen for the He and Ar isotopic analysis of ore-forming fluids, and the first He and Ar isotope data have been obtained from the study region.3He/4He ratios in 14 samples collected from 7 mining districts are 2.17x10-6-12.52×10-6, averaging 6.86×10-6 and their R/Ra ratios are 1.56-9.01 Ra, averaging 4.37 Ra. By projecting the data points onto the 3He-4He concentrations diagram, all the points fall near the mantle helium area. The calculated mantle-source helium ratios are within the range of 19.58%-76.96%, with an average of 49.52%. Argon isotopic characteristics are close to those of mantle source, indicating that the ore-forming material was transport upwards via the multi-stage evolution of mantle plume and concentrated as ores in the favorable loci of mantle branch structures.
机译:近年来,尽管在关于成矿作用和成矿物质来源方面仍存在一些争议,但大兴安岭岭中南段的矿石勘探取得了长足的进步。选择了Pb-Zn-Ag矿床进行成矿流体的He和Ar同位素分析,并从研究区域获得了第一个He和Ar同位素数据。从7个矿山中采集的14个样品中的3He / 4He比区域为2.17x10-6-12.52×10-6,平均6.86×10-6,R / Ra比为1.56-9.01 Ra,平均为4.37 Ra。通过将数据点投影到3He-4He浓度图上,所有点都落在地幔氦区域附近。计算得出的地幔源氦比率在19.58%-76.96%的范围内,平均值为49.52%。氩同位素特征接近地幔源,表明成矿物质是通过地幔柱的多阶段演化而向上输送的,并作为矿石集中在地幔分支结构的有利位置。

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