Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Patrycja Bogusz"'
Autor:
Jolanta Gałazka-Friedman, Martyna Jakubowska, Patrycja Bogusz, Katarzyna Brzózka, Agnieszka Grabias, Rafał Idczak, Robert Konieczny, Tadeusz Szumiata, Marek Woźniak, Miroslav Maslan, Łukasz Karwowski
Publikováno v:
Hyperfine Interactions. 243
Space agencies are working on the project of capturing asteroids which contain natural resources valuable for industry. Based on studies of meteorites samples it was determined that the most useful source of raw materials for this purpose could be pa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::96ced8dddbe553c0f29ff9ea32822c97
https://doi.org/10.1007/s10751-022-01808-z
https://doi.org/10.1007/s10751-022-01808-z
Autor:
Jolanta Gałązka-Friedman, Martyna Jakubowska, Marek Woźniak, Patrycja Bogusz, Łukasz Karwowski, Przemysław Duda
4M method is a new application of Mössbauer spectroscopy to quantitative classification of ordinary chondrites. 4M derives from four words: meteorites, Mössbauer spectroscopy, multidimensional discriminant analysis, Mahalanobis distance. This metho
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c518ffc8780616eb7d47afc41b0e83b9
http://hdl.handle.net/20.500.12128/22245
http://hdl.handle.net/20.500.12128/22245
Autor:
Martyna Jakubowska, Jolanta Gałązka-Friedman, Marek Woźniak, Patrycja Bogusz, Łukasz Karwowski, Przemysław Duda
Mössbauer spectra of nonweathered ordinary chondrites consist of four main mineral phases: olivines, pyroxenes, metallic phase and troilite. These minerals represent more than 95% of the whole mass of an ordinary chondrite. Distribution of these min
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1f4f82a75a9987a2ddd69058f69db42c
http://hdl.handle.net/20.500.12128/22292
http://hdl.handle.net/20.500.12128/22292
Autor:
Łukasz Karwowski, Marek Woźniak, Patrycja Bogusz, Martyna Jakubowska, Jolanta Gałązka-Friedman, Przemysław Duda
Classification of the meteorites is very complex, but in general all meteorites can be divided into three groups: stony, iron and stony-iron. Ordinary chondrites are the most numerous group among stony meteorites. In this paper, we present short revi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::89bb52fd56fdb6797206b022f884f598
http://hdl.handle.net/20.500.12128/13011
http://hdl.handle.net/20.500.12128/13011
Autor:
Patrycja Bogusz, Marek Woźniak, B. Górka, Jolanta Gałązka-Friedman, Tadeusz Szumiata, Katarzyna Brzózka
Publikováno v:
Acta Physica Polonica A. 134:1070-1075
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dc6eae893ac3a59093de6b49518a1964
https://doi.org/10.12693/aphyspola.134.1070
https://doi.org/10.12693/aphyspola.134.1070
Autor:
Martyna Jakubowska, Marek Woźniak, Katarzyna Brzózka, Patrycja Bogusz, Jolanta Gałązka-Friedman, Łukasz Karwowski, Przemysław Duda
Publikováno v:
Hyperfine Interactions. 240
In our paper four Mӧssbauer spectra of ordinary chondrites (previously classified by a classical method based on determining the ratio of ferrosilite (Fs) to fayalite (Fa) with an electron microprobe) are presented and discussed. These are the Mӧss
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e78989d01518b8383b8867b5362d482d
https://doi.org/10.1007/s10751-019-1659-7
https://doi.org/10.1007/s10751-019-1659-7