22 citations as recorded by crossref.

1. Diamond in the Oceanic Lithosphere. Volcanic Diamonds and Diamonds in Ophiolites E. Galimov & F. Kaminsky 10.1134/S0016702921010043
2. The characteristics of Ib diamond crystals synthesized in a Fe–Ni–C system with different SiC contents Y. Wang et al. 10.1039/D1CE00590A
3. Characterization of the nitrogen state in HPHT diamonds grown in an Fe–C melt with a low sulfur addition A. Yelisseyev et al. 10.1039/D2CE00487A
4. Heat-conducting properties of thermobarically-sintered detonation nanodiamond V. Plotnikov et al. 10.22226/2410-3535-2022-4-350-353
5. Orientational Dependences of Diamonds Grown in the NiMnCo–Silicate–H2O–C System under HPHT Conditions and Implications to Natural Diamonds Z. Lu et al. 10.1021/acsearthspacechem.1c00381
6. Raman Spectroscopy of Impact Popigai Astrobleme Diamonds Heat Treated at 5.5 GPa A. Chepurov et al. 10.1007/s10891-022-02638-0
7. Composition of Volatiles Captured by Diamonds during Growth in the Metal–Carbon–Silicate System at High Pressure and High Temperature A. Tomilenko et al. 10.1134/S0016702921080085
8. Morphology of Crystals Growing in Impact Diamonds of the Popigai Astrobleme (Experimental Data) A. Chepurov et al. 10.1134/S1028334X21090063
9. Modern Concepts on Diamond Genesis F. Kaminsky & S. Voropaev 10.1134/S0016702921110033
10. Crystallization of Diamonds and Phase Composition of the FeNi–Graphite–CaCO3 System at 5.5 GPa: the Role of Subduction in Their Formation V. Sonin et al. 10.1134/S1075701523030042
11. Diamond growth and characteristics in the metal-silicate-H2O-C system at HPHT conditions Z. Lu et al. 10.1016/j.lithos.2021.106470
12. DIAMOND CRYSTALLIZATION AND PHASE COMPOSITION IN THE FeNi – GRAPHITE – CaCO3 SYSTEM AT 5.5 Gpa V. Sonin et al. 10.31857/S0016777023030048
13. Patterns of Phase Formation in Kimberlite under Reducing Conditions at 4 GPa and 1500°C E. Zhimulev et al. 10.1134/S1028334X22060162
14. Solid-State Transformations of Mayenite and Core-Shell Structures of C12A7@C Type at High Pressure, High Temperature Conditions S. Gromilov et al. 10.3390/ma16052083
15. Growth rate and morphology study of tetrahydrofuran hydrate single crystals and the effect of salt N. Ismail & C. Koh 10.1039/D2CE00176D
16. Where did the largest diamonds grow? The experiments on percolation of Fe-Ni melt through olivine matrix in the presence of hydrocarbons A. Chepurov et al. 10.1016/j.lithos.2021.106437
17. Studying the Stability of the K/Ar Isotopic System of Phlogopites in Conditions of High T, P: 40Ar/39Ar Dating, Laboratory Experiment, Numerical Simulation D. Yudin et al. 10.3390/min11020192
18. Crystallogenetic Causes of the Unique Shape of the Matryoshka Diamond: The Effect of Capturing a Diamond Inclusion of Twin Diamond Crystals A. Pavlushin & D. Konogorova 10.1134/S0016702923030102
19. Crystallogenetic Causes of the Unique Shape of the Matryoshka Diamond: The Effect of Capturing a Diamond Inclusion of Twin Diamond Crystals A. Pavlushin & D. Konogorova 10.31857/S001675252303010X
20. HPHT-Treated Impact Diamonds from the Popigai Crater (Siberian Craton): XRD and Raman Spectroscopy Evidence A. Chepurov et al. 10.3390/min13020154
21. Details of Interaction between CaCO3 and Fe at 4 GPa and 1400‒1500°C E. Zhimulev et al. 10.1134/S1028334X22600268
22. Surface Porosity of Natural Diamond Crystals after the Catalytic Hydrogenation A. Chepurov et al. 10.3390/cryst11111341