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Diamonds and Highly Reduced Minerals from Chromitite of the Ray-IzOphiolite of the Polar Urals: Deep Origin of Podiform Chromititesand Ophiolitic Diamonds
Authors:YANG 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.
Affiliation:CARMA, State Key Laboratory of Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy ofGeological Sciences, Beijing 100037, China;GFZ, Helmholtz Zentrum Potsdam, 14473 Potsdam, Germany;GFZ, Helmholtz Zentrum Potsdam, 14473 Potsdam, Germany;CCFS/GEMOC, Earth and Planetary Sciences, Macquarie University, NSW 2109 Australia;CARMA, State Key Laboratory of Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy ofGeological Sciences, Beijing 100037, China;CARMA, State Key Laboratory of Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy ofGeological Sciences, Beijing 100037, China;CARMA, State Key Laboratory of Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy ofGeological Sciences, Beijing 100037, China;CARMA, State Key Laboratory of Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy ofGeological Sciences, Beijing 100037, China;Institute of Geology, Komi Scientific Center of Ural Division, RAS, Syktyvkar, 167982, Russia;Institute of Geology, Komi Scientific Center of Ural Division, RAS, Syktyvkar, 167982, Russia
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