Zobrazeno 1 - 8
of 8
pro vyhledávání: '"E. N. Grib"'
Publikováno v:
Petrology, 27 (3). pp. 243-264.
This paper reports the results of a study of naturally and experimentally quenched melt inclusions in magnesian olivine (Fo77–89) from a basalt sample from the Karymsky volcanic center, which is located in the middle segment of the Eastern Volcanic
Publikováno v:
Journal of Volcanology and Seismology. 9:81-103
This paper is the first attempt at a detailed description of petrographic, mineralogical, and geochemical features for the rock complex that makes the Bol’shoi Semyachik volcanic massif (BSVM). The massif was formed in three phases: the pre-caldera
Autor:
E. N. Grib, V. L. Leonov
Publikováno v:
Journal of Volcanology and Seismology. 8:1-16
We provide new evidence that bears on the geological structure, history of evolution, and structural setting for the Bol’shoi Semyachik Volcanic Massif in Kamchatka. The new Ar-Ar results for dating of volcanic rocks allowed significant advances in
Publikováno v:
Journal of Volcanology and Seismology. 6:301-315
Variation in the geochemical characteristics of basalts has been found within the Karymskii Volcanic Center (KVC). The concentrations of potassium, titanium, phosphorus, large-cation, high-charge, rare and rare-earth elements increase from the fronta
Publikováno v:
Journal of Volcanology and Seismology. 3:367-387
This paper is concerned with the petrology and geochemistry of rocks found in the Karymskii Volcanic Center (KVC), which is the largest volcanic center in the Eastern volcanic belt of Kamchatka. The KVC has been built in a rhythmic manner since the L
Autor:
E. N. Grib, A. B. Perepelov
Publikováno v:
Journal of Volcanology and Seismology. 2:228-247
The olivine basalts of the Karymskii Volcanic Center (KVC) can be traced during the history of the area from the Lower Pleistocene until recently (the 1996 events); they are typical low-and moderate-potassium tholeiite basalts of the geochemical isla
Publikováno v:
Petrology. 16:1-18
Melt inclusions were examined in phenocrysts in basalt, andesite, dacite, and rhyodacite from the Karymskii volcanic center in Kamchatka and dacite form Golovnina volcano in Kunashir Island, Kuriles. The inclusions were examined by homogenization and
Publikováno v:
Materials for Renewable and Sustainable Energy, Vol 8, Iss 1, Pp 1-13 (2019)
Abstract The influence of the surface modification of multi-walled carbon nanotubes (MWCNT) with nitrogen-containing compounds on the performance of 40 wt% Pt/MWCNT catalysts in the oxygen electroreduction reaction (ORR) was investigated using a rota
Externí odkaz:
https://doaj.org/article/a817de3915d44f439f4907ddc7211b47