Zobrazeno 1 - 4
of 4
pro vyhledávání: '"I. N. Buchnev"'
Autor:
T. M. Skovitina, A. B. Kotov, D. V. Lopatin, V. P. Kovach, I. N. Buchnev, E. V. Adamskaya, O. V. Bobrovskaya
Publikováno v:
Doklady Earth Sciences. 510:248-252
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::33511690e24926390231d2d9d67d4c61
https://doi.org/10.1134/s1028334x2360007x
https://doi.org/10.1134/s1028334x2360007x
Autor:
S. D. Velikoslavinskii, T. M. Skovitina, A. B. Kotov, E. V. Adamskaya, V. P. Kovach, Viktor A. Gorovoy, I. N. Buchnev
Publikováno v:
Doklady Earth Sciences. 499:616-618
Sm–Nd isotope–geochemical studies of the Cenozoic sand deposits of the Muya Depression (eastern flank of the Baikal rift zone), which is located on the border of the Charo–Olekminskii Geoblock of the Aldan Shield and the Anamakit–Muya Zone of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0ad33822ac4db523bc77455105a5b8cc
https://doi.org/10.1134/s1028334x21080055
https://doi.org/10.1134/s1028334x21080055
Autor:
B. M. Gorokhovskii, I. N. Buchnev, E. V. Tolmacheva, V. P. Kovach, D. V. Lopatin, А. B. Kotov, Eugene V. Sklyarov, T.V. Donskaya, T. M. Skovitina, Yu. V. Plotkina
Publikováno v:
Доклады Академии наук. 484:325-328
U–Th–Pb geochronological (LA-ICP-MS) stady the detritе zircons from the Late Cainozoic sands of the Olkhon island (the Baikal rift zone) were performed. It is shown that the early Paleozoic magmatic and metamorphic complexes of the Olkhon terrei
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::01fa170044873a29ff8dd1a139319845
https://doi.org/10.31857/s0869-56524843325-328
https://doi.org/10.31857/s0869-56524843325-328
Autor:
D. V. Lopatin, T. M. Skovitina, B. M. Gorokhovskii, T.V. Donskaya, I. N. Buchnev, E. V. Tolmacheva, V. P. Kovach, A. B. Kotov, Eugene V. Sklyarov, Yu. V. Plotkina
Publikováno v:
Doklady Earth Sciences. 484:45-47
Geochronological (LA–ICP–MS) U–Th–Pb studies of detrital zircon of the Late Cenozoic sand deposits on Ol’khon Island have been performed. It has been shown that their main source is represented by Early Paleozoic igneous and metamorphic com
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fed77f615316dd76396b8bf8e0f78b33
https://doi.org/10.1134/s1028334x19010203
https://doi.org/10.1134/s1028334x19010203