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Murzinka massif in the Middle Urals as an example of an interformational granite pluton: magmatic sources, geochemical zonation, peculiarities of formation
Murzinka massif constitutes an interformational sheet-like body reaching up 6 km in length steeply dipping to the east. Proterozoic metamorphic rocks of predominantly granulite facies (p = 5–6 kbar, T = 750–800℃) occur at the base of the massif, with Silurian-Devonian volcanic-sedimentary rocks meta...
Tallennettuna:
| Päätekijät: | , |
|---|---|
| Aineistotyyppi: | Artigo |
| Kieli: | Inglês |
| Julkaistu: |
A.N. Zavaritsky Institute of Geology and Geochemistry
2020-05-01
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| Sarja: | Литосфера |
| Aiheet: | |
| Linkit: | https://www.lithosphere.ru/jour/article/view/1267 |
| Tagit: |
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