Origin of high-Fe liquid in magmatic processes: evidence from mid-Paleoproterozoic Elet’ozero titaniferous syenite-gabbro complex (Northern Karelia, Russia)

Evgenii Vitalievich Sharkov, Maria M. Bogina and Alexei V. Chistyakov, Institute of Geology of Ore De, Moscow, Russia
Back to: Volumes, Timescales, and Frequency of Magmatic Processes in Plutons, Chambers, and Reservoirs in the Earth's Crust III Posters