Geochemistry International is a journal of cosmochemistry; geochemistry of magmatic, metamorphic, hydrothermal, and sedimentary processes; organic geochemistry; applied geochemistry; and chemistry of the environment. Geochemistry International provides readers with a unique opportunity to refine their understanding of the geology of the vast territory of the Eurasian continent.
Factors of 18O/16O fractionation in corundum estimated from the calculation of isotopic shifts on vibration frequencies
Coronitic textures in the ferrogabbroids of the Elet’ozero intrusive complex (northern Karelia, Russia) as evidence for the existence of Fe-rich melt. 1. Types of coronas
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