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- W3148265581 abstract "Petrographical 和 geochemical 方法被联合调查起源， geodynamic 和 Shurijeh 沙岩的捱过的历史， Kopet-Dagh 盆。pointcounting 方法和 XRF 技术被用于形式并且 geochemical 分析。把考试基于 petrographical，看起来， Shurijeh 沙岩主要在 craton 被扔内部、再循环的 orogen 带。除了 petrographical 调查，近来侏罗记早的白垩纪摇的 geochemical 分析(主要氧化物和踪迹元素) 表明沉积过程在被动大陆人边缘被执行。如此的解释与 geodynamic 和 Kopeh-Dagh 盆的 paleogeographical 研究被支持在期间这次。geochemical 调查建议可能的来源岩石的作文主要与次要的 mafic 是酸中介的火的岩石。基于上面， Paleo-Tethys 残余和他们的碰撞相关的 granitoids，在马什哈德的南方和西方，可以是为这些岩石的来源区域。中央情报局价值，在样品从 63.8 ～ 94.9 ，正在建议一对改变的相对高的度中等(捱过) 在来源区域。因此， siliciclastic 岩石的 petrographical 和 paleogeographical 研究能在来源区域被用于起源，构造背景和 paleoweathering 研究。" @default.
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- W3148265581 date "2013-01-01" @default.
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- W3148265581 title "Detrital Mode and Geochemistry of the Shurijeh Formation （Late Jurassic-Early Cretaceous） in the Central and Western Parts of the Intracontinental Kopet-Dagh Basin, NE Iran： Implications for Provenance, Tectonic Setting and Weathering Processes" @default.
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