首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Application of enzyme leach soil analysis for epithermal gold exploration in the Andes of Ecuador
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Application of enzyme leach soil analysis for epithermal gold exploration in the Andes of Ecuador

机译:酶浸土壤分析在厄瓜多尔安第斯山脉超热金矿勘探中的应用

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摘要

Enzyme Leach(SM) (EL) soil surveys were undertaken over known epithermal Au mineralisation at El Mozo and Llano Largo, Azuay, Ecuador to assess the utility of the technique for identifying such deposits in the Ecuadorian Andes. The results indicate the development of both apical- and oxidation-type EL anomalies over auriferous structures at the two sites, the former systematically incorporating Au, and the latter Cl and Br. The spectrum of elements responsive to mineralisation at El Mozo (Cl, Br, I, La, Ce, Nd, Cu, Pb, Au, As, Sb, Ag, Zr, Sr) was found to be considerably greater than at Llano Largo (Cl, Br, Au, As, Sb, Ag, Zn), probably reflecting the contrasting high- and low-sulphidation assemblages of the two prospects. Ratios of EL versus aqua-regia extractable trace element concentrations ranged from 1: < 100 for Mn to 1: > 400 for chalcophile elements such as Pb, Sb, As, Bi and Ag. Strong correlations between the concentrations of several analytes (including Mn, Sr, Cu, Cc, As) extracted by the two procedures indicate, however, that EL datasets are extensively influenced by bulk matrix composition. Spatial variations of EL extractable Mn were found to exert no major influence on apical or oxidation suite anomaly patterns at El Mozo. However, Mn-normalisation of halogen data for Llano Largo elucidated otherwise obscure oxidation features, potentially related to Au mineralisation, Ratios between elements subject to apical enrichment and those of the oxidation suite (e.g. Cl/Au and Bi/Br) were found to highlight known Au targets with improved clarity. The formation mechanism of the recorded Au anomalies is uncertain, but may involve physical enrichment of Au in the soil during pedogenesis with subsequent in-situ formation of (EL soluble) Au halide complexes. The strength of such apical features is, in part, probably a function of the minimal depths to mineralisation which characterise El Mozo and Llano Largo. Oxidation halos formed by volatile non-metallic elements such as Cl and Br may, therefore, provide more valuable EL pathfinders for more deeply concealed epithermal targets. (C) 2002 NERC. Published by Elsevier Science Ltd. All rights reserved. [References: 22]
机译:在厄瓜多尔阿苏伊州的艾尔莫佐和拉诺拉尔戈,对已知的超热金矿化进行了酶浸(SM)土壤调查,以评估该技术在厄瓜多尔安第斯山脉中识别此类沉积物的实用性。结果表明,在这两个位置的前期结构上,尖峰型和氧化型EL异常的发展,前者系统地结合了Au,而后者Cl和Br。发现在El Mozo(Cl,Br,I,La,Ce,Nd,Cu,Pb,Au,As,Sb,Ag,Zr,Sr)对矿化有响应的元素光谱要比在Llano Largo( Cl,Br,Au,As,Sb,Ag,Zn),可能反映了两种前景的高硫和低硫组合。 EL与水域可提取微量元素的浓度之比范围从Mn的1:<100到亲硫性元素(如Pb,Sb,As,Bi和Ag)的1:> 400。通过两种方法提取的几种分析物(包括Mn,Sr,Cu,Cc,As)的浓度之间具有很强的相关性,这表明EL数据集受到整体基质组成的广泛影响。发现EL可萃取Mn的空间变化对El Mozo的顶部或氧化套件异常模式没有重大影响。然而,Llano Largo的卤素数据的Mn归一化阐明了其他模糊的氧化特征,可能与Au矿化有关,发现顶端富集元素与氧化套件元素之间的比率(例如Cl / Au和Bi / Br)突出显示已知的金靶具有更高的清晰度。所记录的金异常的形成机理尚不确定,但可能涉及在成岩过程中土壤中金的物理富集以及随后的(EL可溶性)金卤化物复合物的原位形成。这种顶端特征的强度在某种程度上可能是最小化矿化深度的函数,而最小化矿化深度是El Mozo和Llano Largo的特征。因此,由挥发性非金属元素(例如Cl和Br)形成的氧化晕可能为更深层隐藏的超热目标提供更有价值的EL探路者。 (C)2002 NERC。由Elsevier Science Ltd.出版。保留所有权利。 [参考:22]

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