机译:阿魏酸酯酶中铬的氧逸度和价态:Cr〜(2+)是否可以作为深层地幔的氧化还原指示剂?
Geochemical Research Center, Graduate School of Science, The University of Tokyo, Hongo, Tokyo 113-0033, Japan;
Geochemical Research Center, Graduate School of Science, The University of Tokyo, Hongo, Tokyo 113-0033, Japan;
Department of Geoscience, Shizuoka University, Ohya, Shizuoka 422-8529, Japan;
Department of Multidisciplinary Sciences, Graduate School of Arts and Sciences, The University of Tokyo, Komaba, Tokyo 153-8902, Japan;
Department of Multidisciplinary Sciences, Graduate School of Arts and Sciences, The University of Tokyo, Komaba, Tokyo 153-8902, Japan;
Department of Geoscience, Graduate School of Science, The University of Tokyo, Hongo, Tokyo 113-0033, Japan;
Department of Geoscience, Graduate School of Science, The University of Tokyo, Hongo, Tokyo 113-0033, Japan;
Ferropericlase; Chromium; Valence; Oxygen fugacity; Mantle;
机译:阿魏酸酯酶中铬的氧逸度和价态:Cr 2 + sup>是否可以作为深层地幔的氧化还原指示剂?
机译:阿魏酸铁的三价铁含量与组成,氧逸度,温度和压力的关系:下地幔金刚石形成过程中氧化还原条件的影响
机译:从两种氧化还原代理中占主导地位考古环境披风的证据,以及深层底层外壳的低氧气不足
机译:氧化还原耦合的特征氧气不足适用于玻璃熔炼氧化还原状态的分析
机译:上部地幔的氧气不足的变化
机译:冒纳凯阿火山熔岩的氧化还原变化夏威夷羽羽的氧气逸度以及火山气体在地球氧合作用中的作用
机译:铁铁酶中铬和价铬的氧气性和价态:CAN CR2 +是深层地幔的氧化还原指标吗?