Compositions of chromite, associated minerals, and parental magmas of podiform chromite deposits: The role of slab contamination of asthenospheric melts in suprasubduction zone environments
Podiform chromitites in the mantle sections of ophiolites belong to either high-Cr (metallurgical) or high-Al (refractory) varieties. Their highly variable compositions are reflected by different Cr#s [100Cr/(Cr+Al)] and Cr2O3 and Al2O3 contents of the chromite, falling in the boninitic and MORB fie...
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Published in | Gondwana research Vol. 26; no. 1; pp. 262 - 283 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
01.07.2014
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Subjects | |
Online Access | Get full text |
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