YANG J.S.
CARMA, State Key Laboratory of Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaWIRTH R.
GFZ, Helmholtz Zentrum Potsdam, 14473 Potsdam, GermanyWIEDENBECK M.
GFZ, Helmholtz Zentrum Potsdam, 14473 Potsdam, GermanyGRIFFIN W.L.
CCFS/GEMOC, Earth and Planetary Sciences, Macquarie University, NSW 2109 AustraliaMENG F.C.
CARMA, State Key Laboratory of Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaCHEN S.Y
CARMA, State Key Laboratory of Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaBAI W.J.
CARMA, State Key Laboratory of Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaXU X.X.
CARMA, State Key Laboratory of Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaMAKEEYEV A.B.
Institute of Geology, Komi Scientific Center of Ural Division, RAS, Syktyvkar, 167982, RussiaBRYANCHANINIOVA N.I.
Institute of Geology, Komi Scientific Center of Ural Division, RAS, Syktyvkar, 167982, RussiaYANG J. S.,WIRTH R.,WIEDENBECK M.,GRIFFIN W. L.,MENG F. C.,CHEN S. Y, BAI W. J.,XU X. X.,MAKEEYEV A. B.,BRYANCHANINIOVA N. I.2015. Diamonds and Highly Reduced Minerals from Chromitite of the Ray-Iz Ophiolite of the Polar Urals: Deep Origin of Podiform Chromitites and Ophiolitic Diamonds[J]. Acta Geologica Sinica(),89(z2):107
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