Garnet-glaucophane schists of Tashlinsky block from Maksyutov complex (Southern Urals)
On the basis of newest mineralogical, petrological and isotope-geochemical data we have considered the condition and the nature of garnet-glaucophane schists, associated with antigorite serpentinites. This rocks are localized in the lower part of antigorite serpentinites, which was never observed in...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
A.N. Zavaritsky Institute of Geology and Geochemistry
2015-10-01
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| Series: | Литосфера |
| Subjects: | |
| Online Access: | https://www.lithosphere.ru/jour/article/view/213 |