The redox state in the Fizh mantle section, the northern Oman ophiolite as an analog of mantle wedge in subduction zone
The redox state in the Fizh mantle section, the northern Oman ophiolite as an analog of mantle wedge in subduction zone
复制标题
Fizh地幔剖面的氧化还原状态，阿曼北部蛇绿岩是俯冲带地幔楔的类比
DOI：
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发表时间：
2016
期刊：
影响因子：
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通讯作者：
Masafumi Tani,Eiichi TAKAZAWA,Madhusoodhan Satish-Kumar,Masahide Akasaka,Yoshihiko Tamura
中科院分区：
文献类型：
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作者：
Uno;K.;Furukawa;K.;Ando;H.;Shinmura;T.;Miyoshi;M.;Masafumi Tani,Eiichi TAKAZAWA,Madhusoodhan Satish-Kumar,Masahide Akasaka,Yoshihiko Tamura
