Oxygen fugacity and valence state of chromium in ferropericlase: Can Cr^ be a redox indicator for the deep mantle?
Oxygen fugacity and valence state of chromium in ferropericlase: Can Cr^ be a redox indicator for the deep mantle?
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方镁石中铬的氧逸度和价态:Cr^ 可以作为深部地幔的氧化还原指示剂吗?
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发表时间:
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影响因子:
0.7
通讯作者:
Takashi Mikouchi
中科院分区:
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作者:
Hiroyuki Kagi;Shoko Odake;Hidemi Ishibashi;Katsumi Shozugawa;Motoyuki Matsuo;Wataru Satake;Takashi Mikouchi