Библиография
Вулкан:
Группировать:  
Выбрать:     Все     A     B     C     D     E     F     G     H     I     J     K     L     M     N     O     P     R     S     T     V     W     Y     Z     А     Б     В     Г     Д     Е     Ж     З     И     К     Л     М     Н     О     П     Р     С     Т     У     Ф     Х     Ц     Ч     Ш     Щ     Э     Я     
Записей: 64
Страницы:  1 2 3 4 5 6 7
 B
Barmina G.S., Ariskin A.A., Neilsen R.L., Ozerov A.Yu. Formation of high-Al basalt by polybaric fractionation of a high-magnesia parent: Klyuchevskoi volcano (Kamchatka, Russia) / AGU Spring Meeting 1995. Eos Trans. Abstract V42A-06. Baltimore, Maryland, USA: AGU. 1995. P. 298
Bazanova L.I., Puzankov M.Yu., Maksimov A.P. Plinian basaltic andesite eruptions of Avachinsky volcano, Kamchatka, Russia: chronology, dynamics and deposits // European Geosciences Union 2007. 2007. Vol. 9. P. 05012
Bazhenova O.K., Arefiev O.A., Frolov E.B. Oil of the volcano Uzon caldera, Kamchatka // Organic Geochemistry. 1998. Vol. 29. № 1–3. P. 421 - 428. doi: 10.1016/S0146-6380(98)00129-6.
   Аннотация
There are reported gas chromatography, gas chromatography/mass spectrometry and carbon isotopic data on the oils sampled in caldera of the Uzon volcano (East Kamchatka). The Uzon volcano is located in the west of the eastern Kamchatka basin which is made up of thick Paleogene-Neogene sedimentary rocks. Its caldera is made up of lacustrine volcanogenic-sedimentary formations of Pleistocene age (38–70 thousand years), lying on dense basalts. Two samples studied were heavy oils (0.915 g/ml) and contained 2 sulfur; 2.5 paraffin, 9.3 waxes; 1.4 wt olefinic hydrocarbons. Their gas chromatograms show a mono-modal distribution for n-alkanes with a maximum at C18. Pristane/Phytane concentration ratios were measured to be 0.48–0.52. Olefinic hydrocarbons were interpreted to be of hydrothermal origin. Sterane and triterpane biomarkers indicated a low maturation degree and a lacustrine orgin of the initial organic matter. The Uzon oil was found to be isotopically heavy with a δ13C value of −21‰14C isotope was detected, which indicates that recent plant organic matter was significantly involved in oil generation process.
Belousov A. B. Distribution and eruptive mechanism of maars in the Kamchatka Peninsula // Doklady Earth Sciences. 2006. Vol. 406. № 1. P. 24-27. doi:10.1134/S1028334X06010077.
Belousov A., Belousova M. Dynamics and viscosity of 'a'a and pahoehoe lava flows of the 2012-13 eruption of Tolbachik volcano, Kamchatka, Russia // Bulletin of Volcanology. 2018. Vol. 80. № 6.
Belousov A., Belousova M., Kozlov D. The distribution of tephra deposits and reconstructing the parameters of 1973 eruption on Tyatya volcano, Kunashir, Kurile Islands // Journal of Volcanology and Seismology. 2017. Vol. 11. № 4. P. 285-294.
Belousov A., Belousova M., Nechayev A. Video observations inside conduits of erupting geysers in Kamchatka, Russia, and their geological framework: Implications for the geyser mechanism // Geology. 2013. Vol. 41. № 4. P. 387-390. doi:10.1130/G33366.1.
Belousov A., Belousova M., Voight B. Tsunamis Generated by Subaquatic Volcanic Explosions: Unique Data from 1996 Eruption in Karymskoye Lake, Kamchatka, Russia // Pure and Applied Geophysics. 2000. Vol. 157. № 6-8. P. 1135-1143. doi:10.1007/s000240050021.
Belousov A.B. The Shiveluch volcanic eruption of 12 November 1964 — explosive eruption provoked by failure of the edifice // Journal of Volcanology and Geothermal Research. 1995. Vol. 66. № 1-4. P. 357-365. doi:10.1016/0377-0273(94)00072-O.
Belousov Alexander Deposits of the 30 March 1956 directed blast at Bezymianny volcano, Kamchatka, Russia // Bulletin of Volcanology. 1996. Vol. 57. № 8. P. 649-662. doi:10.1007/s004450050118.