Solid-state redistribution of mineral particles in the upwelling mantle flow as a mechanism of chromite concentration in the ophiolite ultramafic rocks (on the example of Kraka ophiolite, the Southern Urals)
The main regularities of the structure of chromitite-bearing zones of ultramafic rock of the ophiolitic association are considered on the example of Kraka massifs. In all studied chromitite-bearing zones, olivine demonstrates a strong preferably crystallographic orientation, indicating that plastic...
| Príomhchruthaitheoirí: | , |
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| Formáid: | Alt |
| Teanga: | English |
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Georesursy Ltd.
2019-03-01
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| Sraith: | Georesursy |
| Ábhair: | |
| Rochtain ar líne: | https://geors.ru/archive/article/961/ |