Murzinka massive at the middle urals as an example of the interformational granite pluton: magmatic sources, geochemical zonality, peculiarities of formation
Murzinka massif is a sheet-like interformational body steeply deeping to the East with length about 6 km. Proterozoic metamorphic rocks of the predominantly granulite facies ( P = 5-6 kbar, T = 750-800°C) occur at the base of massif, and volcanic-sedimentary Silurian-Devonian rocks metamorphosed in...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
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A.N. Zavaritsky Institute of Geology and Geochemistry
2018-10-01
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| Series: | Литосфера |
| Subjects: | |
| Online Access: | https://www.lithosphere.ru/jour/article/view/247 |