22 citations as recorded by crossref.

1. Composition of garnet and clinopyroxene in peridotite xenoliths from the Grib kimberlite pipe, Arkhangelsk diamond province, Russia: Evidence for mantle metasomatism associated with kimberlite melts A. Kargin et al. 10.1016/j.lithos.2016.07.015
2. Alakit and Daldyn kimberlite fields, Siberia, Russia: Two types of mantle sub-terranes beneath central Yakutia? I. Ashchepkov et al. 10.1016/j.gsf.2016.08.004
3. Ilmenite as a recorder of kimberlite history from mantle to surface: examples from Indian kimberlites J. Xu et al. 10.1007/s00710-018-0616-5
4. Thermobarometry and Geochemistry of Mantle Xenoliths from Zapolyarnaya Pipe, Upper Muna Field, Yakutia: Implications for Mantle Layering, Interaction with Plume Melts and Diamond Grade I. Ashchepkov et al. 10.3390/min10090755
5. Reconstructions of mantle structure beneath the Anabar Shield kimberlites – similarities and differences I. Aschepkov et al. 10.1016/j.geogeo.2024.100282
6. Comparative mineralogy, geochemistry and petrology of aillikites and carbonatites, ijolites, melteigites and Ne-syenites of Beloziminsky massif- insights to origin I. Ashchepkov et al. 10.1016/j.geogeo.2024.100309
7. The Dynamics of Transformation of Lithospheric Mantle Rocks Beneath the Siberian Craton Y. Perepechko et al. 10.3390/min13030423
8. MANTLE TERRANES OF THE SIBERIAN CRATON: THEIR INTERACTION WITH PLUME MELTS BASED ON THERMOBAROMETRY AND GEOCHEMISTRY OF MANTLE XENOCRYSTS I. Ashchepkov et al. 10.5800/GT-2019-10-2-0412
9. Reconstructions of lithospheric mantle beneath Aldan shield based on deep-seated xenocrysts from lamprophyres of Chompolo field, Russia I. Ashchepkov et al. 10.1007/s12040-021-01694-z
10. Eclogite Varieties and Their Positions in the Cratonic Mantle Lithosphere beneath Siberian Craton and Archean Cratons Worldwide I. Ashchepkov et al. 10.3390/min12111353
11. A genetic relationship between magnesian ilmenite and kimberlites of the Yakutian diamond fields S. Kostrovitsky et al. 10.1016/j.oregeorev.2020.103419
12. Aillikites and Alkali Ultramafic Lamprophyres of the Beloziminsky Alkaline Ultrabasic-Carbonatite Massif: Possible Origin and Relations with Ore Deposits I. Ashchepkov et al. 10.3390/min10050404
13. Incompatible element-enriched mantle lithosphere beneath kimberlitic pipes in Priazovie, Ukrainian shield: volatile-enriched focused melt flow and connection to mature crust? I. Ashchepkov et al. 10.1080/00206814.2020.1761893
14. Interaction between protokimberlite melts and mantle lithosphere: Evidence from mantle xenoliths from the Dalnyaya kimberlite pipe, Yakutia (Russia) I. Ashchepkov et al. 10.1016/j.gsf.2016.05.008
15. Trace element geochemistry of mantle xenoliths from Zarnitsa kimberlite pipe, Daldyn field, Yakutia: Complex history of melts interactions with lithospheric mantle I. Ashchepkov et al. 10.1016/j.geogeo.2024.100313
16. Deep mantle roots of the Zarnitsa kimberlite pipe, Siberian craton, Russia: Evidence for multistage polybaric interaction with mantle melts I. Ashchepkov et al. 10.1016/j.jseaes.2021.104756
17. Thermobarometry of diamond inclusions: Mantle structure and evolution beneath Archean cratons and mobile belts worldwide I. Ashchepkov et al. 10.1016/j.geogeo.2022.100156
18. High-precision EPMA measurement of trace elements in ilmenite and reference material development L. Jia et al. 10.1039/D2JA00238H
19. Ilmenite from the Arkhangelsk Diamond Province, Russia: Composition, Origin and Indicator of Diamondiferous Kimberlites A. Kargin et al. 10.1134/S0869591120040050
20. Origin of clinopyroxene-ilmenite symplectites in mafic granulites from eastern parts of the Chotanagpur granite gneissic complex, East Indian shield S. Chatterjee et al. 10.2138/am-2022-8715
21. The formation of saline mantle fluids by open-system crystallization of hydrous silicate-rich vein assemblages – Evidence from fluid inclusions and their host phases in MARID xenoliths from the central Kaapvaal Craton, South Africa J. Konzett et al. 10.1016/j.gca.2014.10.015
22. Experimental Research on Electrical Conductivity of the Olivine-Ilmenite System at High Temperatures and High Pressures W. Sun et al. 10.3389/feart.2022.861003