About the genesis of ovoidal K-feldspar and porphyry quartz in rapakivi granites and related rocks
DOI:
https://doi.org/10.21638/11701/spbu07.2017.101Abstract
A comparative study of structural peculiarities of ovoid K-feldspar porphyry and quartz of rapakivi granite of different arrays (Aland, Vyborg, Salmi batholith rapakivi of the Baltic shield and Bardiaush batholith rapakivi of the South Ural), and hybrid rocks of various genesis allowed us to clarify their role in the formation of rapakivi granite complexes.
It was established, that the porphyritic quartz and ovoides of K-feldspar and their plagioclase shell was formed before the crystallization of the residual cotectic melt of rapakivi granite. In the composite hybrid magmatic rocks xenocryst K-spar have undergone a disintegration of solid solution with formation of a secondary cryptoperthite plagioclase. And xenocrystic quartz was subject to decrepitation by primary fluid inclusions and the formation of new secondary high-temperature inclusions. In a hybrid composite rocks formed as metamorphic and basic igneous rocks ovoid-like porphyroblast Kspar (including plagioclase shells) and quartz porphyry (including the ‘ocelly’) was crystallized from solution. In the crystals of quartz primary inclusions (negative crystals) of trigonal symmetry were present, typical for low-temperature α-modification. Refs 24. Figs 9. Tables 2.
Keywords:
granite rapakivi, ovoides, porphyroblast, hybrid rocks, metasomatic rocks
Downloads
References
References
Downloads
Published
How to Cite
Issue
Section
License
Articles of "Vestnik of Saint Petersburg University. Earth Sciences" are open access distributed under the terms of the License Agreement with Saint Petersburg State University, which permits to the authors unrestricted distribution and self-archiving free of charge.