Sapphire-bearing magmatic rocks trace the boundary between paleo-continents: A case study of Ilmenogorsky alkaline complex, Uralian collision zone of Russia

Author:

Sorokina Elena S.,Botcharnikov Roman E.,Kostitsyn Yuri A.,Rösel Delia,Häger Tobias,Rassomakhin Mikhail A.,Kononkova Nataliya N.,Somsikova Alina V.,Berndt Jasper,Ludwig Thomas,Medvedeva Elena V.,Hofmeister Wolfgang

Funder

Council on grants of the President of the Russian Federation

Ministry of Science and Higher Education of the Russian Federation

Deutscher Akademischer Austauschdienst

Alexander von Humboldt-Stiftung

Johannes Gutenberg-Universität Mainz

Publisher

Elsevier BV

Subject

Geology

Reference97 articles.

1. Petrogenesis of alkaline basalt-hosted sapphire megacrysts. Petrological and geochemical investigations of in situ sapphire occurrences from the Siebengebirge Volcanic Field, Germany;Baldwin;Contrib. Mineral. Petrol.,2017

2. Igneous zircon: trace element compositon as an indicator of source rock type;Belousova;Contrib. Mineral. Petrol.,2002

3. Ruby and sapphire from Jegdalek, Afghanistan;Bowersox;Gems Gemol.,2000

4. Mountain building processes during continent–continent collision in the Uralides;Brown;Earth Sci. Rev.,2008

5. Isotope geochronology of alkaline rocks of the Urals in the light of zircon uranium-lead data;Chernyshev;Geochemistry,1987

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