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Oxygen fugacity and valence state of chromium in ferropericlase: Can Cr2+ be a redox indicator for the deep mantle?

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？

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Hiroyuki KAGI; Shoko ODAKE; Hidemi ISHIBASHI; Katsumi SHOZUGAWA; Motoyuki MATSUO; Wataru SATAKE; Takashi MIKOUCHI;
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1. Oxygen fugacity and valence state of chromium in ferropericlase: Can Cr2+ be a redox indicator for the deep mantle? [J] . Hiroyuki KAGI, Shoko ODAKE, Hidemi ISHIBASHI, Journal of mineralogical and petrological sciences . 2013,第3期

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？
2. Oxygen fugacity and valence state of chromium in ferropericlase: Can Cr~(2+) be a redox indicator for the deep mantle? [J] . Hiroyuki Kagi, Shoko Odake, Hidemi Ishibashi, Journal of Mineralogical and Petrological Sciences . 2013,第3期

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？
3. Ferric iron content of ferropericlase as a function of composition, oxygen fugacity, temperature and pressure: Implications for redox conditions during diamond formation in the lower mantle [J] . Otsuka K., Longo M., McCammon C.A., Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System . 2013,第Null期

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
4. Characteristic oxygen fugacity of redox couples in glass applied to the analysis of the redox state of glass melts [C] . O. Pinet, C. di Nardo American Ceramic Society . 2000

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
5. Variations in the Oxygen Fugacity of the Upper Mantle [D] . Birner, Suzanne K. 2018

机译：上部地幔的氧气不足的变化
6. Redox variations in Mauna Kea lavas the oxygen fugacity of the Hawaiian plume and the role of volcanic gases in Earth’s oxygenation [O] . Maryjo Brounce, Edward Stolper, John Eiler 2017

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
7. Evidence for a dominantly reducing Archaean ambient mantle from two redox proxies, and low oxygen fugacity of deeply subducted oceanic crust [O] . Sonja Aulbach, Alan B. Woodland, Richard A. Stern, 2019

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

Oxygen fugacity and valence state of chromium in ferropericlase: Can Cr2+ be a redox indicator for the deep mantle?

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