Zobrazeno 1 - 4
of 4
pro vyhledávání: '"I. Ye. Starik"'
Publikováno v:
Annals of the New York Academy of Sciences. 91:576-582
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::800b14a21c691d80fe6650517213517b
https://doi.org/10.1111/j.1749-6632.1961.tb35524.x
https://doi.org/10.1111/j.1749-6632.1961.tb35524.x
Autor:
E. V. Sobotovich, I. Ye. Starik
Publikováno v:
International Geology Review. 7:142-150
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0d90609412241341fe0d24cc81a93b1f
https://doi.org/10.1080/00206816509474096
https://doi.org/10.1080/00206816509474096
Publikováno v:
International Geology Review. 5:804-811
Analyses were made of samples of the several classes of iron meteorites: (hexahedrites, octahedrites, ataxites, and troilite inclusions) in further study of the isotopic composition of primordial lead and toward establishing correlation between the d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::337189a0a914c9905003a54101bad91d
https://doi.org/10.1080/00206816309473821
https://doi.org/10.1080/00206816309473821
Autor:
A. V. Lovtsyus, E. V. Sobotovich, S.M. Grashchenko, I. Ye. Starik, M. M. Shats, G. P. Lovtsyus
Publikováno v:
International Geology Review. 6:2100-2109
The time of consolidation, differentiation, and breakup of the parent bodies of meteorites are considered. The age of the substance of stony and iron meteorites are calculated on the basis of uranium, lead, and lead isotope composition. It is conclud
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3a9c02cffa31e9a4f7d057ba67618409
https://doi.org/10.1080/00206816409474697
https://doi.org/10.1080/00206816409474697