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Problems Involved in Using Improper Calibration CRMs in Geochemical Analyses: A Case Study on Mafic Rocks of Boggulakonda Pluton, East of Cuddapah Basin, India

机译:在地球化学分析中使用不正确的校准CRM涉及的问题:以印度Cuddapah盆地东部Boggulakonda Pluton的镁铁质岩为例

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摘要

The performance and response of two commonly used certified reference materials (CRMs) for mafic rocks MRG-1 (CANMET, Canada) and JGb-1 (Geological Survey of Japan), both gabbroic in composition, are evaluated for a set of mafic plutonic rocks (gabbros) from Boggulakonda (BK) occurring to the east of Proterozoic Cuddapah Basin, South India. In this study, quadrupole-inductively coupled plasma mass spectrometry was used to generate trace and rare earth element (REE) data using MRG-1 and JGb-1 as calibration standards separately for a comparative study. It is found that the two CRMs show highly variable major, minor and trace element compositions except ΣREE. When used for BK gabbros, JGb-1 has yielded better results than MRG-1 with respect to trace elements (HFS elements Nb and Ta in specific), whereas a good agreement was observed between both CRMs for REE concentrations when compared with certified data. The Nb–Ta element distribution patterns for BK gabbros in the spidergrams plotted using JGb-1 as CRM show relatively prominent and pronounced negatively spiking anomalies with reference to Th, whereas using MRG-1 as calibration CRM yielded unresolved and unclear Nb–Ta anomalies in the present study. The geochemistry (major, minor and trace) of MRG-1 is different when compared to that of JGb-1. Probably this is reason for the disparity in the results obtained by inductively coupled plasma mass spectrometry on mafic plutonic rocks. The study conducted on the BK gabbros, reveals better and reliable results using JGb-1 as CRM. This study also reveals the importance of using proper CRM for calibration having closely matching trace and REE concentrations in addition to major and minor elements, for obtaining reliable data in geological samples.
机译:对一组镁铁质深成岩评价了镁铁质岩石的两种常用认证参考材料(CRM)MRG-1(加拿大CANMET)和JGb-1(日本地质调查局)的性能和响应(gabros)来自Boggulakonda(BK),发生在印度南部元古代Cuddapah盆地东部。在这项研究中,使用四极电感耦合等离子体质谱法分别使用MRG-1和JGb-1作为校准标准来生成痕量和稀土元素(REE)数据,以进行比较研究。发现这两个CRM显示出除ΣREE以外的高度可变的主要,次要和微量元素组成。当用于BK长颈鹿时,就痕量元素(特别是HFS元素Nb和Ta)而言,JGb-1的结果优于MRG-1,而与认证数据相比,两种CRM的REE浓度均观察到良好的一致性。使用JGb-1作为CRM绘制的蜘蛛图中BK长颈鹿的Nb-Ta元素分布模式相对于Th显示出相对突出和明显的负尖峰异常,而使用MRG-1作为校准CRM则产生了未解决和不清楚的Nb-Ta异常。本研究。与JGb-1相比,MRG-1的地球化学(主要,次要和痕量)不同。这可能是由于在镁铁质深部岩石上通过电感耦合等离子体质谱法获得的结果不一致的原因。在BK长颈鹿上进行的研究揭示了使用JGb-1作为CRM的更好,更可靠的结果。这项研究还揭示了使用适当的CRM进行校准的重要性,该校准除了主要元素和次要元素外还具有痕量的REE和REE浓度,以确保地质样品中可靠的数据。

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