Conditions of crystallization of granites and pegmatites of Tarbaganakhsky massif (Kuluarsky ridge, Verkhoyanye)
Compression during granite crystallization in the anticline arch leads to the formation of fluid- gneiss structures and separation of remanent pegmatite melt with its further moving to the periphery of the complex. Two-staged crystalfization is enhanced by presence of Ca in the melt. The early stage...
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| Autors principals: | , |
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| Format: | Artigo |
| Idioma: | Russo |
| Publicat: |
Sergo Ordzhonikidze Russian State University for Geological Prospecting
2015-02-01
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| Col·lecció: | Известия высших учебных заведений: Геология и разведка |
| Matèries: | |
| Accés en línia: | https://www.geology-mgri.ru/jour/article/view/4 |
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