...
  • 主题
高级搜索  >
历史搜索 清空历史
首页> 外文期刊>International journal of applied environmental sciences >Petrography and Geochemistry of Urf suite from Aqaba complex, Southern Jordan
【24h】

Petrography and Geochemistry of Urf suite from Aqaba complex, Southern Jordan

机译：Petrography and Geochemistry of Urf suite from Aqaba complex, Southern Jordan

获取原文
获取原文并翻译 | 示例
           
页面导航
  • 摘要
  • 著录项
  • 相关主题

摘要

The Aqaba complex located at the south-eastern of Jordan, exposes coexisting mafic-felsic association typical of syn- to pre-plate collision magmatism. The bulk of the pluton is made of quartz monzonite, granite and granodiorite. New U-Pb zircon dating revealed a synchronous emplacement of the granite (605 ± 4.6 and 617 ± 3.7 Ma), granodiorite (613 ± 4.4, 612 ± 3.6 and 611.8 ± 4.9 Ma) and quartz monzonite (608 ± 5.4 Ma). The whole-rock geochemistry indicate that the source for the quartz monzonite, granite and granodiorites could have been a continental arc-derived from mantle sources and mature metagreywackes. Melting of this crustal material was subduction related , which could have been an enriched mantle-derived melt contaminated . The Aqaba complex is a part of a the Arabian-Nubian Shield (ANS) are juvenile in character, Neoproterozoic, including in addition five large plutonic suites; Rahma, Darba, Rumman,Urf and Yutum suite. The genesis of these suites were likely induced by mantle-derived magma in the shallow crust while their spatially and temporally discrete emplacement at shallow levels was probably related to the (extensional) of lithospheric boundaries, which represent a feasible fertile source for such granitoids.

著录项

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