Zobrazeno 1 - 10
of 12
pro vyhledávání: '"A. D. Babansky"'
Autor:
M. L. Tolstykh, A. D. Babansky, M. D. Smirnova, M. M. Pevzner, V. A. Lebedev, Yu. O. Larionova, Yu. V. Kushcheva, A. V. Parfenov
Publikováno v:
Journal of Volcanology and Seismology. 17:119-133
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fb3739b365ca09bccd830ec24bb9d710
https://doi.org/10.1134/s0742046323700100
https://doi.org/10.1134/s0742046323700100
Publikováno v:
Geochemistry International. 59:139-155
Melt inclusions were investigated in the minerals of dacite tephra of the largest Holocene eruption (7900 years) of Khangar volcano, Sredinny Range of Kamchatka. Melt compositions correspond to rhyolite (SiO2 = 70–77 wt %, Na2O+K2O = 6–7 wt %) wi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::13c92f03641f98bd21f015ee11b486df
https://doi.org/10.1134/s0016702921020087
https://doi.org/10.1134/s0016702921020087
Autor:
A. D. Babansky, Yu. V. Kuscheva, M. L. Tolstykh, M. M. Pevzner, Vladimir A. Lebedev, Yu. A. Kostitsin, A. O. Volynets, Yu. V. Gol’tsman
Publikováno v:
Russian Geology and Geophysics. 61:700-714
—We report the chemical and isotopic compositions of volcanic rocks of the Akhtang and Kostina mountain massifs in the Sredinny Range, Kamchatka. The analyzed rocks are similar in composition to the earlier studied volcanics of the eastern flank of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::63974c7d9e177c38832d20ecce9de76d
https://doi.org/10.15372/rgg2019158
https://doi.org/10.15372/rgg2019158
Autor:
Vladimir A. Lebedev, M. L. Tolstykh, M. M. Pevzner, Yu. A. Kostitsin, A. D. Babansky, A. O. Volynets
Publikováno v:
Doklady Earth Sciences. 489:1413-1416
K-Ar isotopic age of the beginning of formation of Ichinsky (0,35 Ma) and Khangar (0,4 Ma) stratovolcanoes is established for the first time, as well as the age of the final stage of activity of the Lauchan Ridge (about 0,9 Ma) in the Sredinny Range
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::456abac6322a3d8d964d6c57c1ad8950
https://doi.org/10.1134/s1028334x19120213
https://doi.org/10.1134/s1028334x19120213
Autor:
Vladimir A. Lebedev, M. M. Pevzner, A. O. Volynets, M. L. Tolstykh, A. D. Babansky, Yu. V. Kuscheva
Publikováno v:
Doklady Earth Sciences. 490:1-3
A first set of K–Ar isotopic ages obtained, which allowed to estimate the age of the largest volcanoes of the Anaunsky Dol (3.2, 2.2 and 1.9 Ma) and eruptive centers of the post-caldera stage of Uksichan massif (1.2 and 0.8 Ma), located in the Sred
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1219cfac2e857cfe6569ec8a93141b32
https://doi.org/10.1134/s1028334x20010080
https://doi.org/10.1134/s1028334x20010080
Publikováno v:
Геохимия. 64:237-262
This paper presents the results of a study of melt inclusions in plagioclase, amphibole and pyroxene from Ichinsky volcano’s tephras of different age. Two types of melts have been identified, distinguished by different concentrations of potassium (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a062bf0ab427e5f8cef30dfb8cc3cf89
https://doi.org/10.31857/s0016-7525643237-262
https://doi.org/10.31857/s0016-7525643237-262
Publikováno v:
Geochemistry International. 57:243-265
The paper reports data on glassy melt inclusions in minerals of tephra that was produced by the most significant eruptions of Ichinsky volcano, Kamchatka, and marked the major evolutionary stages of the volcanic center in the Pleistocene–Holocene.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::02dc3cdc2a4f150ebcfb63e4d7e8b609
https://doi.org/10.1134/s0016702919030121
https://doi.org/10.1134/s0016702919030121
Publikováno v:
Russian Geology and Geophysics. 59:1577-1591
Based on the geochemical characteristics of the Miocene–Quaternary volcanic rocks of the Sredinny Range of Kamchatka, we divide it into northern and southern provinces; the latter comprises the “eastern”, “western”, and “central” flanks
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0639c48dc03cdcf52434ef07ceaf9153
https://doi.org/10.1016/j.rgg.2018.12.004
https://doi.org/10.1016/j.rgg.2018.12.004
Publikováno v:
Journal of Volcanology and Seismology. 12:242-251
It is shown that Shiveluch, which consists of several volcanic edifices that stand in one area and in part overlie each other, is a long-lived volcanic massif with a complex structure. The available data on the morphology of the edifice, age, rock co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cf1cf764f5ccead143dca862933acdb4
https://doi.org/10.1134/s0742046318040061
https://doi.org/10.1134/s0742046318040061
Autor:
Yu. A. Kostitsin, Yu. V. Kushcheva, M. L. Tolstykh, M. M. Pevzner, A. D. Babansky, Vladimir A. Lebedev, D. V. Kovalenko, A. O. Volynets
Publikováno v:
Doklady Earth Sciences. 475:858-862
For the first time, the age of the beginning of the volcanic activity within Sredinny metamorphic Massif is determined (7–6 Ma). We suppose that this event was caused by the collision of Kamchatka with the Kronotsk arc that started about 7 Ma from
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5336584b1968e52fb3d77edce38233e0
https://doi.org/10.1134/s1028334x17080189
https://doi.org/10.1134/s1028334x17080189