Abstract
The Ragozinka crater, 9 km in diameter and located in the Middle Urals, had been a debatable object for a long time until its impact origin was established. It is expressed by a circular negative gravity anomaly surrounded by positive ring anomaly of the rim zone.
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Reference
Vishnevsky, S. A. (1999). Ragozinka: Eocenian marine impact crater on the middle Urals, Russia. Meteoritics & Planetary Science, 34(4), A117.
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Komatsu, G., Coletta, A., Battagliere, M.L., Virelli, M. (2019). Ragozinka, Russia. In: Flamini, E., Di Martino, M., Coletta, A. (eds) Encyclopedic Atlas of Terrestrial Impact Craters. Springer, Cham. https://doi.org/10.1007/978-3-030-05451-9_47
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DOI: https://doi.org/10.1007/978-3-030-05451-9_47
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