PETROLOGICAL EVIDENCES OF SYNDEFORMATION SEGREGATION OF CHROMITES DURING DUNITE FORMATION: EXAMPLE OF KRAKA OPHIOLITES, SOUTH URALS
Results of structural and mineralogical studies of chromitite-bearing zone localized in spinel peridotites of the Middle Kraka ophiolite massif are presented. The rocks of the studied area are characterized by deformation structures, which are cuased by plastic flow under high-PT conditions. Olivine...
I tiakina i:
| Ngā kaituhi matua: | , , , , |
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| Hōputu: | Artigo |
| Reo: | Inglês |
| I whakaputaina: |
South Urals Federal Research Center of Mineralogy and Geoecology UB RAS
2016-12-01
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| Rangatū: | Минералогия |
| Ngā marau: | |
| Urunga tuihono: | https://journal.mineralogy.ru/wp-content/uploads/2019/09/2016-4-5.pdf |
| Ngā Tūtohu: |
Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!
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