{"title":"喀尔巴阡盆地陨石的重新评估:Kisvarsány, Knyahinya, Mezőmadaras, Mike, Mócs和Nyírábrány的初步结果","authors":"I. Kubovics, Z. Puskás, K. Gál-Sólymos","doi":"10.1556/AGEOL.47.2004.2-3.10","DOIUrl":null,"url":null,"abstract":"Magnetic spherules from Pleistocene terrestrial sediments in southern Hungary were systematically collected and investigated. By means of chemical analysis, Fe, Fe(Mn), Fe(Ni) and glassy (silicate) spherules can be distinguished. Some of them have characteristic features suggesting an extraterrestrial origin: Ni-bearing crust, Ni-rich core and especially the platinum group nuggets with their unique chemical composition. They could have been formed by meteorite ablation process.","PeriodicalId":107929,"journal":{"name":"Acta Geologica Hungarica","volume":"2 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2004-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":"{\"title\":\"Re-evaluation of meteorites from the Carpathian Basin: Preliminary results from Kisvarsány, Knyahinya, Mezőmadaras, Mike, Mócs and Nyírábrány\",\"authors\":\"I. Kubovics, Z. Puskás, K. Gál-Sólymos\",\"doi\":\"10.1556/AGEOL.47.2004.2-3.10\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Magnetic spherules from Pleistocene terrestrial sediments in southern Hungary were systematically collected and investigated. By means of chemical analysis, Fe, Fe(Mn), Fe(Ni) and glassy (silicate) spherules can be distinguished. Some of them have characteristic features suggesting an extraterrestrial origin: Ni-bearing crust, Ni-rich core and especially the platinum group nuggets with their unique chemical composition. They could have been formed by meteorite ablation process.\",\"PeriodicalId\":107929,\"journal\":{\"name\":\"Acta Geologica Hungarica\",\"volume\":\"2 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2004-12-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Acta Geologica Hungarica\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1556/AGEOL.47.2004.2-3.10\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Acta Geologica Hungarica","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1556/AGEOL.47.2004.2-3.10","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Re-evaluation of meteorites from the Carpathian Basin: Preliminary results from Kisvarsány, Knyahinya, Mezőmadaras, Mike, Mócs and Nyírábrány
Magnetic spherules from Pleistocene terrestrial sediments in southern Hungary were systematically collected and investigated. By means of chemical analysis, Fe, Fe(Mn), Fe(Ni) and glassy (silicate) spherules can be distinguished. Some of them have characteristic features suggesting an extraterrestrial origin: Ni-bearing crust, Ni-rich core and especially the platinum group nuggets with their unique chemical composition. They could have been formed by meteorite ablation process.
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