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- W3150087319 abstract "迟了的白垩纪 Khabr Marvast tectonized ophiolite 位于 Nain Baft ophiolite 带的中间的部分，在中央伊朗的微大陆的西南的边。尽管在学习区域的所有暴烈的岩石显示subduction相关的 magmatism (例如高 LILE (大离子亲石元素元素)/ HFSE (高领域 strenght 元素)在 Nb 和 Ta 的比率和否定异例)，地质并且 geochemical 数据清楚地在 tectonized 协会区分暴烈的岩石的二个不同的组：(1 ) 组 1 由 hyaloclastic 角砾岩，玄武岩的枕头熔岩，和安山岩表流动组成。这些岩石代表 Nain Baft 海洋的外壳；并且(2 ) 组 2 是从 ophiolite 套房的最高的节的碱的熔岩。这些熔岩显示出 shoshonite 亲密关系，但是不支持 ophiolite 的倾向。" @default.
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- W3150087319 date "2009-01-01" @default.
- W3150087319 modified "2023-09-28" @default.
- W3150087319 title "Petrogenesis of Volcanic Rocks in the Khabr-Marvast Tectonized Ophiolite： Evidence for Subduction Processes in the South-Western Margin of Central Iranian Microcontinent" @default.
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