中国西南宣威组底部粘土岩中REE-Nb的非均质分布:LA-ICP-MS制图的启示

IF 3.6 2区 地球科学 Q1 GEOLOGY
Yuan-Can Ying , Hai-Jun Yu , Wen-Chang Li , De-Zong Li , Dong-Hui Wang , Fang-Yue Wang , Wei Chen , Shao-Yong Jiang
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引用次数: 0

摘要

中国西南地区宣威组(晚二叠世)底部广泛发育REE-Nb-Zr-Ga多金属成矿层,是一种潜在的重要成矿资源。然而,这些元素在不同地层中的分布模式以及它们与粘土矿物的关系仍然是个谜。利用TIMA和LA-ICP-MS填图分析,对宣威组富铁粘土岩(下)和上覆富铝粘土岩(上)的矿物学和地球化学特征进行了研究,揭示了稀土、铌的分布规律及其与粘土矿物的空间关系。结果表明,稀土和铌主要富集于富铝粘土岩中,富铁粘土岩中稀土和铌含量较低。稀土元素富集在富铝粘土岩边界和富铁粘土岩顶部。铌主要存在于铁钛氧化物相和富钛高岭石中。TIMA和LA-ICP-MS图谱显示REE-Nb富集与特定高岭石类型相关。稀土和铌主要富集在高岭石基质中,通常与大量粘土矿物碎片共存。然而,这些碎片本身不包含REE。值得注意的是,在富钛高岭石碎片中,Nb与Ti的耦合关系大于与REE的耦合关系。特别是在富铁粘土岩中,富钛高岭石碎片是铌的主要寄主相,而稀土则被耗尽。相反,在富al粘土岩中,粘土矿物碎片主要由薄铝石组成,薄铝石是一种贫REE、Nb和Zr的相,但却是Ga的主要寄主。这项研究为这些资源的工业利用潜力提供了重要的见解,并为未来的勘探和开采提供了指导。高温煅烧显著提高了稀土酸浸效率,促进了稀土的绿色高效提取。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

The heterogeneous distribution of REE-Nb in the claystone at the bottom of Xuanwei Formation, southwestern China: Insights from LA-ICP-MS mapping

The heterogeneous distribution of REE-Nb in the claystone at the bottom of Xuanwei Formation, southwestern China: Insights from LA-ICP-MS mapping
The REE-Nb-Zr-Ga polymetallic mineralization layers are extensively developed at the bottom of the Xuanwei Formation (Late Permian) in southwestern China and regarded as a potentially significant resource. However, the distribution patterns of these elements across different layers and their association with clay minerals remain enigmatic. This study employs TIMA and LA-ICP-MS mapping analyses to investigate the mineralogical and geochemical characteristics of the Fe-rich claystone (lower part) and the overlying Al-rich claystone (upper part) of the Xuanwei Formation, revealing the distribution patterns of REE and Nb, as well as their spatial relationship with clay minerals. Our results demonstrate that REE and Nb mainly enrich in Al-rich claystone, with lower contents in Fe-rich claystone. The highest REE concentrations occur at the Al-rich claystone boundaries and at the top of the Fe-rich claystone. Nb is predominatly in Fe-Ti oxide phases and Ti-rich kaolinite. TIMA and LA-ICP-MS mapping reveals REE-Nb enrichment correlates with specific kaolinite types. REE and Nb are primarily concentrated in kaolinite matrix, which commonly coexists with numerous clay mineral fragments. However, these fragments themselves do not contain REE. Notably, Nb exhibits a coupled relationship with Ti rather than REE in Ti-rich kaolinite fragments. Especially in Fe-rich claystone, Ti-rich kaolinite fragments constitute the dominant host phase for Nb while being depleted in REE. Conversely, in Al-rich claystone, clay mineral fragments are mainly composed of boehmite, a phase depleted in REE, Nb and Zr, but it is the principal host for Ga. This study gives critical insights into the potential for industrial utilization of these resources and guide for future exploration and extraction. Moreover, high-temperature calcination significantly enhances the acid leaching efficiency of REEs, promoting green and efficient extraction.
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来源期刊
Ore Geology Reviews
Ore Geology Reviews 地学-地质学
CiteScore
6.50
自引率
27.30%
发文量
546
审稿时长
22.9 weeks
期刊介绍: Ore Geology Reviews aims to familiarize all earth scientists with recent advances in a number of interconnected disciplines related to the study of, and search for, ore deposits. The reviews range from brief to longer contributions, but the journal preferentially publishes manuscripts that fill the niche between the commonly shorter journal articles and the comprehensive book coverages, and thus has a special appeal to many authors and readers.
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