Abstract
The Iso-Naakkima structure in eastern Finland was found on the basis of a strikingly circular negative Bouguer gravity anomaly and later verified as an impact crater by drilling results.
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References
Järvelä, J., Pesonen, L. J., & Pietarinen, H. (1995). On palaeomagnetism and petrophysics of the Iso-Naakkima impact structure, southeastern Finland. Geological Survey of Finland, v. Report Q19/29.1/3232/95/1, p. 55.
Pesonen, L. J., Järvelä, J., Sarapää, O., & Pietarinen, H. (1996). The Iso-Naakkima meteorite impact structure: Physical properties and paleomagnetism of a drill core (abstract). Meteoritics & Planetary Science, 31, A105–A106.
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Staffieri, S., Coletta, A., Battagliere, M.L., Virelli, M. (2019). Iso-Naakkima, Finland. 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_91
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DOI: https://doi.org/10.1007/978-3-030-05451-9_91
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