Olivine-chrome-spinel equilibrium in chromitites and ultramafites of Rai-Iz massif, Polar Urals
Olivine and chrome-spinel compositions from chromitites and ore-bearing metamorphosed ultramafic rocks of Rai-Iz massif were compared. It was established that olivine and spinel ferruginosity are directly proportional and increase monotonically from chromitites to ultramafic rocks that indicates the...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
A.N. Zavaritsky Institute of Geology and Geochemistry
2016-01-01
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| Series: | Литосфера |
| Subjects: | |
| Online Access: | https://test.lithosphere.ru/jour/article/view/19 |