Abstract
Indications of impact that confirmed the nature of the Logoisk structure are the presence of shatter cones in the fragments of granite-gneisses and dolomites, the presence of planar structure and deformation lamellae in mineral, coesite and stishovite, and of microcrystal of impact diamond in impactite—suevites.
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References
Gerasimov, M.V., Yakovlev, O.I., Dikov, Y.P., & Wlotzka, F. (2005). Evaporative differentiation of impact-produced melts; laser-simulation experiments and comparison with impact glasses from the Logoisk Crater. Special Paper—Geological Society of America, 385, 351.
Veretennikov, N. V. (2010). The Logoisk impact crater. AIP Conference Proceedings, 1205, 185.
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Staffieri, S., Coletta, A., Battagliere, M.L., Virelli, M. (2019). Logoisk, Belarus. 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_98
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DOI: https://doi.org/10.1007/978-3-030-05451-9_98
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