The crust structure of the Morasko meteorite – a preliminary hypothesis
| dc.contributor.author | Stankowski, Wojciech T.J. | |
| dc.date.accessioned | 2017-06-19T12:53:35Z | |
| dc.date.available | 2017-06-19T12:53:35Z | |
| dc.date.issued | 2017-05 | |
| dc.description.abstract | A 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. | pl_PL |
| dc.identifier.citation | Geologos, 2017, 23, 1, 53-56 | pl_PL |
| dc.identifier.doi | https://doi.org/10.1515/logos-2017-0005 | |
| dc.identifier.isbn | 978-83-232187-4-6 | |
| dc.identifier.issn | 1426-8981 | |
| dc.identifier.uri | http://hdl.handle.net/10593/17936 | |
| dc.language.iso | eng | pl_PL |
| dc.publisher | Instytut Geologii UAM | pl_PL |
| dc.rights | info:eu-repo/semantics/openAccess | pl_PL |
| dc.subject | sintered crust | pl_PL |
| dc.subject | fusion crust | pl_PL |
| dc.subject | genesis | pl_PL |
| dc.subject | SEM | pl_PL |
| dc.subject | EDS | pl_PL |
| dc.title | The crust structure of the Morasko meteorite – a preliminary hypothesis | pl_PL |
| dc.type | Artykuł | pl_PL |