¹Addi Bischoff,¹Markus Patzek,^2,3Stefan T. M. Peters,^4,5Jean-Alix Barrat,²Tommaso Di Rocco,²Andreas Pack,¹Samuel Ebert,¹Christian A. Jansen,⁶Kryspin Kmieciak
Meteoritics & Planetary Science (in Press) Open Access Link to Article [https://doi.org/10.1111/maps.13905]
¹Institut für Planetologie, University of Münster, Wilhelm-Klemm-Str. 10, D-48149 Münster, German
²Universität Göttingen, Geowissenschaftliches Zentrum, Goldschmidtstr. 1, D-37077 Göttingen, Germany
³Museum der Natur Hamburg – Mineralogie, LIB, Grindelallee 48, D-20146 Hamburg, Germany
⁴University of Brest, CNRS, IRD, Ifremer, LEMAR, F-29280 Plouzané, France
⁵Institut Universitaire de France, Paris, 75005 France
⁶Olsza 2, 63-100 Śrem, Kraków, Poland
Published by arrangement with John Wiley & Sons

On July 15, 2021, a huge fireball was visible over Poland. After the possible strewn field was calculated, the first and so far only sample, with a mass of 350 g, was discovered 18 days after the fireball event. The Antonin meteorite was found August 3, 2021, on the edge of a forest close to a dirt road near Helenow, a small suburb of the city of Mikstat. The rock is an ordinary chondrite breccia and consists of equilibrated and recrystallized lithologies. The boundaries between different fragments are difficult to detect, and the lithologies are of petrologic type 5 and type 4. The rock is moderately shocked (S4) and contains local impact melt areas and thin shock veins. The low-Ca pyroxene and olivine are equilibrated (Fs20.6 and Fa24.0, respectively), typical of L chondrites. The L chondrite classification is also supported by O isotope data and the results of bulk chemical analysis. The Ti isotope characteristics confirm that Antonin is related to the noncarbonaceous (NC) meteorites. One of the studied thin sections shows an unusual metal–chondrule assemblage, perhaps indicating that the metal in the chondrite is heterogeneously distributed, which is, however, not clearly visible in the element abundances.