Petrova, E. V., & Grokhovsky, V. I. (2026). The Fusion Crust of Meteorites is the Result of Changes in the Meteoroid Material under the Influence of Atmospheric Ablation. Solar System Research, 60(2), 1. https://doi.org/10.1134/S0038094625601239
Chicago Style (17th ed.) CitationPetrova, E. V., and V. I. Grokhovsky. "The Fusion Crust of Meteorites Is the Result of Changes in the Meteoroid Material Under the Influence of Atmospheric Ablation." Solar System Research 60, no. 2 (2026): 1. https://doi.org/10.1134/S0038094625601239.
MLA (9th ed.) CitationPetrova, E. V., and V. I. Grokhovsky. "The Fusion Crust of Meteorites Is the Result of Changes in the Meteoroid Material Under the Influence of Atmospheric Ablation." Solar System Research, vol. 60, no. 2, 2026, p. 1, https://doi.org/10.1134/S0038094625601239.