...
首页> 外文期刊>Lithos: An International Journal of Mineralogy, Petrology, and Geochemistry >High-pressure metamorphic age and significance of eclogite-facies continental fragments associated with oceanic lithosphere in the Western Alps (Etirol-Levaz Slice, Valtournenche, Italy)
【24h】

High-pressure metamorphic age and significance of eclogite-facies continental fragments associated with oceanic lithosphere in the Western Alps (Etirol-Levaz Slice, Valtournenche, Italy)

机译:西阿尔卑斯山高压岩石的变质年龄和与海洋岩石圈有关的榴辉岩相大陆碎片的意义(意大利瓦尔图尔嫩切,Etirol-Levaz Slice)

获取原文
获取原文并翻译 | 示例
           

摘要

The Etirol-Levaz Slice in the Penninic Alps (Valtournenche, Italy) is a piece of eclogite-facies continental basement sandwiched between two oceanic units, the blueschist-facies Combin Zone in the hanging wall and the eclogite-facies Zermatt-Saar Zone in the footwall. It has been interpreted as an extensional allochthon from the continental margin of Adria, emplaced onto ultramafic and mafic basement of the future Zermatt-Saar Zone by Jurassic, rifting-related detachment faulting, and later subducted together with the future Zermatt-Saas Zone. Alternatively, the Etirol-Levaz Slice could be derived from a different paleogeographic domain and be separated from the Zermatt-Saas Zone by an Alpine shear zone.
机译:Penninic Alps(意大利瓦尔图尔嫩切)的Etirol-Levaz片是一块榴辉岩相的大陆基底,夹在两个海洋单元之间,蓝岩岩相的Combin区位于悬壁中,而榴辉岩相的Zermatt-Saar区位于下盘。它被解释为是阿德里亚大陆边缘的延伸性异位线,被侏罗纪,裂谷相关的剥离断层置于未来的采尔马特-萨尔地带的超镁铁质和镁铁质基底上,随后与未来的采尔马特-萨斯地带一起俯冲。或者,Etirol-Levaz切片可以源自不同的古地理域,并通过高山剪切带与Zermatt-Saas带分开。

著录项

相似文献

  • 外文文献
  • 中文文献
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