首页> 外文OA文献 >Leaching systematics and matrix elimination for the determination of high-precision Pb isotope compositions of ocean island basalts
【2h】

Leaching systematics and matrix elimination for the determination of high-precision Pb isotope compositions of ocean island basalts

机译:测定海洋岛屿玄武岩中高精度Pb同位素组成的浸出系统和基质消除

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

Ocean island basalts from Hawaii and Kerguelen were analyzed for their Pb isotopic compositions to assess the effect of acid leaching and matrix elimination by Pb anion exchange columns on reproducibility and accuracy. Unleached samples consistently yield Pb isotopic ratios that reflect the incorporation of foreign material. Leaching removes up to 70-80% of the total Pb content of the samples with corresponding weight losses between 35 and 60%. The older and more altered Kerguelen basalts show better external reproducibility than the Hawaiian basalts, which appears to be due to the presence in the Hawaiian samples of more radiogenic contaminants (e.g., seawater Pb, drilling mud, and related alteration phases). All leached samples purified twice on anion exchange columns show more radiogenic Pb isotopic ratios than those processed once. The difference is larger for tholeiitic basalts (Hawaiian and Kerguelen Plateau) than for transitional to alkalic basalts (Kerguelen Archipelago). The small differences in measured ratios of total procedural triplicates reflect differential elimination of residual alteration via leaching and matrix effects. The effectiveness of matrix elimination depends on the specific basalt composition, and tholeiitic basalts (i.e., low Pb concentrations) require two passes on anion exchange columns. This study shows that all steps in sample processing are critical for achieving accurate high-precision Pb isotopic compositions of ocean island basalts. © 2009 by the American Geophysical Union.
机译:分析了来自夏威夷和克格伦的大洋玄武岩的Pb同位素组成,以评估酸浸和Pb阴离子交换柱消除基质对重现性和准确性的影响。未浸出样品始终产生反映异物掺入的Pb同位素比率。浸出最多可去除样品中总铅含量的70-80%,相应的重量损失在35%至60%之间。较旧且变化较大的Kerguelen玄武岩显示出比夏威夷玄武岩更好的外部再现性,这似乎是由于夏威夷样品中存在更多的放射源性污染物(例如海水Pb,钻探泥浆和相关的蚀变阶段)。在阴离子交换柱上纯化两次的所有浸出样品均比一次处理的样品具有更高的放射性铅同位素比。对于高渗玄武岩(夏威夷和克尔格伦高原),其差异要大于过渡到碱性玄武岩(克尔格伦群岛)的差异。总程序重复率的测量比率的细微差异反映了通过淋洗和基质效应差异消除了残留变化。基质消除的有效性取决于特定的玄武岩组成,而可塑玄武岩(即低Pb浓度)需要在阴离子交换柱上进行两次通过。这项研究表明,样品处理中的所有步骤对于实现精确的海洋岛玄武岩Pb同位素组成至关重要。 ©2009,美国地球物理联盟。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号