首页> 外文OA文献 >Gamma-ray Spectrometry Of Granite Pegmatite Pegmatitic Province Borborema (ppb), Northeast Brazil [espectrometria De Raios Gama De Granitos Pegmatíticos Da Província Pegmatítica Da Borborema (ppb), Nordeste Do Brasil]
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Gamma-ray Spectrometry Of Granite Pegmatite Pegmatitic Province Borborema (ppb), Northeast Brazil [espectrometria De Raios Gama De Granitos Pegmatíticos Da Província Pegmatítica Da Borborema (ppb), Nordeste Do Brasil]

机译:巴西东北部花岗岩伟晶岩伟晶岩省Borborema(ppb)的伽玛射线光谱法[巴西东北部Borborema伟晶岩岩层(ppb)的花岗岩的伽玛射线光谱法]

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摘要

The objective of this study is the characterization of pegmatitic granites located in the southern region of the Borborema Pegmatitic Province (BPP) with aerial and ground gamma ray data. Ground gamma ray data, radiometric and ICP-MS laboratory analysis showed that these granites have uranium concentrations varying between 0.4 ppm and 7.8 ppm, thorium concentrations varying between 0.1 ppm and 21 ppm and potassium concentrations varying between 2% and 5.2%. Based on these radiometric characteristics and using individual, ratios and ternary images of radioelements of aerial gamma ray data it was possible to distinguish from others country rocks a group of granitic pegmatitic bodies and also to individualize quartzitic formations from the northern and southern portions of the area, based on their different thorium (Th) contents. Ground gamma ray data, acquired for one of these pegmatitic granites, called Galo Branco granite, reveals an irregular spatial distribution of radioelements, indicating mineralogical changes in contents and concentrations of accessory minerals during magmatic crystalization. Pegmatites intruding quartzites in the south portion of the granite were also distinguished using eU/eTh and eU/K ratios images. The results indicated the potential of these methods for the characterization and mapping of pegmatitic granites and associated pegmatites of the Borborema Pegmatitic Province (BPP). © 2010 Sociedade Brasileira de Geofísica.
机译:这项研究的目的是利用航空和地面伽玛射线数据对位于博尔博雷马·培古玛蒂省(BPP)南部地区的古培花岗岩进行表征。地面伽玛射线数据,辐射度和ICP-MS实验室分析表明,这些花岗岩的铀浓度在0.4 ppm至7.8 ppm之间变化,th浓度在0.1 ppm至21 ppm之间变化,钾浓度在2%至5.2%之间变化。基于这些辐射特征,并使用航空伽玛射线数据的放射性元素的个体,比例和三元图像,可以将一组花岗岩岩溶体与其他乡村岩石区分开,并可以区分该地区北部和南部的石英岩层。 ,根据their的含量不同而定。为这些变质岩花岗岩之一(称为Galo Branco花岗岩)获取的地面伽玛射线数据揭示了放射性元素的不规则空间分布,表明岩浆结晶过程中辅助矿物的含量和浓度发生矿物学变化。还使用eU / eTh和eU / K比图像区分了花岗岩南部的伟晶岩侵入石英岩。结果表明,这些方法在表征和绘制Borborema岩溶岩省(BPP)的岩溶岩和相关岩溶岩方面具有潜力。 ©2010巴西地球科学会。

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