Ilmenite in peridotite and pyroxenite xenoliths from Siberian kimberlite pipes: morphology and genesis

Tatiana Kalashnikova; Sophia Vorobey; Sergei Kostrovitsky

doi:https://doi.org/10.5194/egusphere-egu25-11724

[Back] [Session GD2.3]

EGU25-11724, updated on 15 Mar 2025

https://doi.org/10.5194/egusphere-egu25-11724

EGU General Assembly 2025

© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.

Ilmenite in peridotite and pyroxenite xenoliths from Siberian kimberlite pipes: morphology and genesis

Tatiana Kalashnikova

^1,2, Sophia Vorobey³, and Sergei Kostrovitsky¹

Tatiana Kalashnikova et al.

¹Vinogradov Institute of Geochemistry SB RAS, Geochemistry of basic and ultrabasic rock, Irkutsk, Russian Federation (kalashnikova@igc.irk.ru)
²Institute of Earth crust SB RAS, Irkutsk, Russian Federation
³Vernadsky Institute of Geochemistry RAS, Moscow, Russian Federation

How to cite: Kalashnikova, T., Vorobey, S., and Kostrovitsky, S.: Ilmenite in peridotite and pyroxenite xenoliths from Siberian kimberlite pipes: morphology and genesis, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-11724, https://doi.org/10.5194/egusphere-egu25-11724, 2025.

This abstract has been withdrawn on 25 Jul 2025.