首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >Constant Cu/Ag in upper mantle and oceanic crust: Implications for the role of cumulates during the formation of continental crust
【24h】

Constant Cu/Ag in upper mantle and oceanic crust: Implications for the role of cumulates during the formation of continental crust

机译:上部地幔和海洋地壳中的常数Cu / Ag:在欧洲地壳形成过程中对累积作用的影响

获取原文
获取原文并翻译 | 示例
           

摘要

Delamination of dense, sulfide-bearing pyroxenitic cumulates was proposed to explain the low Cu content and the evolved major element composition of the continental crust, yet evidence for this hypothesis has been circumstantial. In this study, we present Cu and Ag contents of mantle pyroxenites and associated peridotites from the Balmuccia peridotite massif (Italian Alps) and mantle xenoliths from Hannuoba (North China Craton) to constrain the fractionation behavior of Cu and Ag during melt-peridotite reaction and magmatic accumulation in the mantle. Furthermore, we reexamine the behavior of these elements during arc magmatism and in other reservoirs to highlight the fractionation of Cu and Ag as an important tracer for processes that led to the formation of continental crust.
机译:提出了致密的硫化硫化物含有硫化硫化物累积,以解释大陆壳的低Cu含量和演进的主要元素组成,但这一假设的证据是个性的。 在这项研究中,我们呈现Cu和Ag含有来自Hannuoba(华北Craton)的Balmuccia PeridoTite Massif(意大利阿尔卑斯山)和甲板的联系的恒星含量,以限制Cu和Ag在熔融恒星反应中的分馏行为和 岩石中的岩石积累。 此外,我们在弧形岩浆中和其他储层中重新审视这些元素的行为,以突出Cu和Ag的分馏作为导致欧洲地壳形成的过程的重要示踪剂。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

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