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Method for Ultra-Low-Level Analysis of Gold in Rocks

机译:岩石中金的超低位分析方法

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A new method for analyzing gold at ultralow concentrations (<10 pg/g) in geological samples has been developed involving HF-aqua regia acid digestion, chromatographic separation of Au from matrix elements using DIBK supported on an inert resin, and analysis by inductively coupled plasma-mass spectrometry (ICPMS). This method has an analytical detection limit of 2 parts per trillion (pg/g), significantly lower than most routinely used methods developed for analysis of ore samples with Au concentrations considerably higher than average crustal abundance (approx2 ng/g). Such methods commonly have detection limits in the low nanogram per gram range. Many areas of geological research including ore genesis, crustal mobility and redistribution, planetary differentiation, and plume volcanism require quantitative analysis of geological materials with much lower Au concentrations. We present a rapid, easy to use method where Au is separated from matrix elements onto extractant primed chromatographic resin and analyzed by quadrupole ICPMS. The method is suitable for the relatively rapid analysis of a large number of samples and is reliable over a wide range of concentrations from picogram to microgram per gram level. Analysis of four different geostandards, GXR1, GXR4, CH-3, and SARM 7, yields concentrations within error of the published concentrations with accuracies of >95percent.
机译:已经开发了一种新的分析地质样品中超低浓度(<10 pg / g)的金的方法,包括HF-王水消化,使用惰性树脂支撑的DIBK色谱分离金与基质元素以及电感耦合分析等离子体质谱法(ICPMS)。该方法的分析检出限为2万亿分之一(pg / g),大大低于开发用于分析金含量远高于平均地壳丰度(约2 ng / g)的矿石样品的大多数常规方法。这样的方法通常具有在每克低纳克范围内的检测极限。地质研究的许多领域,包括矿床成因,地壳迁移和再分布,行星分化和羽状火山作用,都需要对金含量低得多的地质物质进行定量分析。我们提出了一种快速,易于使用的方法,其中将Au与基质元素分离到萃取剂底漆色谱树脂上,并通过四极杆ICPMS分析。该方法适用于大量样品的相对快速分析,并且在从皮克到微克/克的各种浓度范围内均可靠。对四种不同的地理标准(GXR1,GXR4,CH-3和SARM 7)进行分析,得出的浓度在已公布浓度的误差范围内,其准确度> 95%。

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