Stankowski, Wojciech T.J.2017-06-192017-06-192017-05Geologos, 2017, 23, 1, 53-56978-83-232187-4-61426-8981http://hdl.handle.net/10593/17936A small piece of the Morasko meteorite, weighing 970 g, yields traces of its journey through the Earth’s atmosphere and of its impact into a mineral substrate, such as reflected in the meteorite’s crust. This is seen in the crust structure in the form of sintered as well as fusion and semi-fusion layers for which ablative niches are optimum sites. Subsequent weathering processes have resulted in significant mineralogical changes in the crusts. The meteorite crusts originated during polygenetic processes.enginfo:eu-repo/semantics/openAccesssintered crustfusion crustgenesisSEMEDSArtykułhttps://doi.org/10.1515/logos-2017-0005