(Unless otherwise stated, the copyright of the materials included belong to Jan Woreczko & Wadi.)
Szablon:Mirek (2025)
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| - | Mirek Agnieszka, Szopa Krzysztof, Owczarzak Andrzej, Banasik Kamila, (2025), '''Meteoryt [[Kaalijarv]] – co nowego? (''Kaalijarv meteorite – what's new?'')''', ''Acta Soc. Metheor. Polon.'', 16, 2025, s. 33-47 ({{!abs-ilink|Szablon:Mirek (2025)}}).<ref>wyniki badań nowych okazów znalezionych w okresie od listopada 2023 do maja 2024 roku przez Andrzeja Owczarzaka i Filipa Nikodema</ref> Plik {{Link-ASMP|BN=1|60168987}}.<noinclude> | + | Mirek Agnieszka, Szopa Krzysztof, Owczarzak Andrzej, Banasik Kamila, (2025), '''Meteoryt [[Kaalijarv]] – co nowego? (''Kaalijarv meteorite – what's new?'')''', ''Acta Soc. Metheor. Polon.'', 16, 2025, s. 33-47 ({{!abs-ilink|Szablon:Mirek (2025)}}).<ref>wyniki badań nowych okazów meteorytu [[Kaalijarv]] znalezionych w okresie od listopada 2023 do maja 2024 roku przez Andrzeja Owczarzaka i Filipa Nikodema</ref> Plik {{Link-ASMP|BN=1|60168987}}.<noinclude> |
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'''Abstract:''' This publication summarizes the current knowledge about the [[Kaalijarv]] meteorite, with a brief historical outline of the [[Kratery Kaalijärv|craters]], and presents and discusses the latest research results on this meteorite. Kaalijarv belongs to the {{Txt2Img|Kaalijarv_(trace_elements_Ni-Ir).png|IAB group}} and is a coarse-grained octahedrite, and its polished and etched surface reveals Widmanstätten figures. It is composed mainly of {{Txt2Img|Kaalijarv_(Mirek_2025)-fig06.jpg|kamacite}}, with smaller amounts of taenite, {{Txt2Img|Kaalijarv_(Mirek_2025)-fig07.jpg|schreibersite}} and {{Txt2Img|Kaalijarv_(Mirek_2025)-fig08.jpg|rhabdite}}. Current research allowed to identify such phases as {{Txt2Img|Kaalijarv_(Mirek_2025)-fig10.jpg|graphite}}, sphalerite and most probably {{Txt2Img|Kaalijarv_(Mirek_2025)-fig12.jpg|native lead}}, native nickel and/or avaruite, and anhydrous carbonate and/or chlorate.<br />Fragments of the meteorite are found in Estonia, in the southeastern part of the Baltic island of Saaremaa. Meteorites found so far had small masses ranging from a few to several dozen grams. Still, recently, it was possible to recover the main mass of a meteorite, which was [[Kaalijarv/Masa główna|5.7 kg]]. | '''Abstract:''' This publication summarizes the current knowledge about the [[Kaalijarv]] meteorite, with a brief historical outline of the [[Kratery Kaalijärv|craters]], and presents and discusses the latest research results on this meteorite. Kaalijarv belongs to the {{Txt2Img|Kaalijarv_(trace_elements_Ni-Ir).png|IAB group}} and is a coarse-grained octahedrite, and its polished and etched surface reveals Widmanstätten figures. It is composed mainly of {{Txt2Img|Kaalijarv_(Mirek_2025)-fig06.jpg|kamacite}}, with smaller amounts of taenite, {{Txt2Img|Kaalijarv_(Mirek_2025)-fig07.jpg|schreibersite}} and {{Txt2Img|Kaalijarv_(Mirek_2025)-fig08.jpg|rhabdite}}. Current research allowed to identify such phases as {{Txt2Img|Kaalijarv_(Mirek_2025)-fig10.jpg|graphite}}, sphalerite and most probably {{Txt2Img|Kaalijarv_(Mirek_2025)-fig12.jpg|native lead}}, native nickel and/or avaruite, and anhydrous carbonate and/or chlorate.<br />Fragments of the meteorite are found in Estonia, in the southeastern part of the Baltic island of Saaremaa. Meteorites found so far had small masses ranging from a few to several dozen grams. Still, recently, it was possible to recover the main mass of a meteorite, which was [[Kaalijarv/Masa główna|5.7 kg]]. | ||
| - | '''Keywords:''' [[ | + | '''Keywords:''' [[Estonia|Estonian meteorite]], [[Kaalijarv]], Kaali, iron meteorite, native lead, Pb native, avaruite |
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Aktualna wersja na dzień 21:35, 3 maj 2025
Mirek Agnieszka, Szopa Krzysztof, Owczarzak Andrzej, Banasik Kamila, (2025), Meteoryt Kaalijarv – co nowego? (Kaalijarv meteorite – what's new?), Acta Soc. Metheor. Polon., 16, 2025, s. 33-47 (abstrakt).[1] Plik ASMP.
Abstract: This publication summarizes the current knowledge about the Kaalijarv meteorite, with a brief historical outline of the craters, and presents and discusses the latest research results on this meteorite. Kaalijarv belongs to the IAB group and is a coarse-grained octahedrite, and its polished and etched surface reveals Widmanstätten figures. It is composed mainly of kamacite, with smaller amounts of taenite, schreibersite and rhabdite. Current research allowed to identify such phases as graphite, sphalerite and most probably native lead, native nickel and/or avaruite, and anhydrous carbonate and/or chlorate.
Fragments of the meteorite are found in Estonia, in the southeastern part of the Baltic island of Saaremaa. Meteorites found so far had small masses ranging from a few to several dozen grams. Still, recently, it was possible to recover the main mass of a meteorite, which was 5.7 kg.
Keywords: Estonian meteorite, Kaalijarv, Kaali, iron meteorite, native lead, Pb native, avaruite
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