Zobrazeno 1 - 10
of 110
pro vyhledávání: '"G. S. Nikolaev"'
Autor:
G. S. Nikolaev
Publikováno v:
Geochemistry International. 61:24-42
Autor:
I. V. Pshenitsyn, A. A. Ariskin, G. S. Nikolaev, D. V. Korost, V. O. Yapaskurt, E. V. Kislov, S. N. Sobolev, I. V. Kubrakova, O. A. Tyutyunnik
Publikováno v:
Geochemistry International. 60:235-255
Publikováno v:
Advances in Geochemistry, Analytical Chemistry, and Planetary Sciences ISBN: 9783031098826
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d7dfc14362817d782273a964b116e4a0
https://doi.org/10.1007/978-3-031-09883-3_3
https://doi.org/10.1007/978-3-031-09883-3_3
Autor:
G. S. Nikolaev
Publikováno v:
Geochemistry International. 59:491-500
A mechanism is suggested to explain the transport of sulfide material by means of its dissolution and subsequent redeposition under the effect of an ascending infiltrating flow of intercumulus melt during the compaction of cumulates in layered pluton
Publikováno v:
Geochemistry International. 59:156-170
Oxygen isotope composition was studied in 33 monomineralic fractions of olivine from plagioclase lherzolite, dunite, troctolite, and olivine gabbronorite of the Yoko-Dovyren layered massif. The δ18O values of the least altered rocks not contaminated
Autor:
Vasiliy O. Yapaskurt, S. N. Sobolev, Leonid V. Danyushevsky, G. S. Nikolaev, I. V. Pshenitsyn, Marco L. Fiorentini, E. V. Kislov, Alexey A. Ariskin
Publikováno v:
Russian Geology and Geophysics. 61:611-633
—The exposures, structure, mineralogy, and composition of unusual sulfide-bearing troctolites from the Yoko-Dovyren layered intrusion in the northern Baikal area (Russia) are described in detail for the first time. The troctolite succession (referr
Autor:
I. V. Pshenitsyn, S. N. Sobolev, G. S. Nikolaev, Alexey A. Ariskin, Vasiliy O. Yapaskurt, E. V. Kislov, Dmitry Korost
Publikováno v:
Petrology. 28:246-262
The paper presents data on sulfide globules in picrodolerites from a bottom apophysis of the Yoko-Dovyren massif, northern Transbaikalia. Textural features of the rocks indicate that they crystallized at rapid magma cooling. Their composition is simi
Publikováno v:
Geochemistry International. 58:1-10
The effect of variations in the fo, fa, en, fs, di, an and ab components in high-Mg basaltic melts on the topology of the spinel liquidus was quantified by conducting simulations with the new SPINMELT-2.0 model for the spinel–melt equilibrium. It h
Publikováno v:
Доклады Академии наук. 487:78-81
Using a new model of the spinel-melt equilibrium SPINMELT-2.0, the effect of variations of fo-, fa-, en-, fs-, di-, an- and ab-components in high-Mg basaltic melts on the topology of the spinel liquidus was quantified. It has been established that en
Publikováno v:
Doklady Earth Sciences. 487:791-794
The influence of variations in fo-, fa-, en-, fs-, di-, an-, and ab-components in a high-Mg basaltic melt on the topology of the spinellide liquidus was analyzed using the new model of the spinellide–melt equilibrium SPINMELT-2.0. It is shown that