Diamonds and Highly Reduced Minerals from Chromitite of the Ray-Iz Ophiolite of the Polar Urals： Deep Origin of Podiform Chromitites and Ophiolitic Diamonds

The Uralide orogenic belt suture zone extending more is a major early Paleozoic than 3000 km in a N-S direction, and geographically divides Europe from Asia （Chemenda et al., 1997）. Ophiolites, podiform chromitites and high pressure metamorphic rocks are well developed in the orogenic belt （Leech an...

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Bibliographic Details
Published in:Acta geologica Sinica (Beijing) 2015-12, Vol.89 (s2), p.107-107
Main 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.
Format: Article
Language:English
Subjects:
乌拉尔
极地
渊源
矿物
蛇绿岩
豆荚状铬铁矿
还原
钻石
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Summary:The Uralide orogenic belt suture zone extending more is a major early Paleozoic than 3000 km in a N-S direction, and geographically divides Europe from Asia （Chemenda et al., 1997）. Ophiolites, podiform chromitites and high pressure metamorphic rocks are well developed in the orogenic belt （Leech and Ernst, 2000）.
ISSN:1000-9515
1755-6724
DOI:10.1111/1755-6724.12308_64