Zobrazeno 1 - 10
of 19
pro vyhledávání: '"N. V. Surkov"'
Publikováno v:
Геодинамика и тектонофизика, Vol 10, Iss 1, Pp 1-19 (2019)
The number Ka=N/N1 is used to evaluate the thermal power of a plume; N is the thermal power transferred from the plume base to its conduit, and N1 is the thermal power transferred from the plume conduit into the surrounding mantle. At the relative th
Externí odkaz:
https://doaj.org/article/7ebda62db8ac456c93afe60c21871863
Autor:
T. I. Kharitonova, N. V. Surkov
Publikováno v:
Arid Ecosystems. 10:10-16
The article discusses remote methods for the description of the intraseasonal dynamics of soil and vegetation moisture. The field moisture content of the soil and vegetation cover is described by an integral indicator that takes into account the mois
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::784fc0550b9fbb3dc9ad5655514c54a1
https://doi.org/10.1134/s2079096120010096
https://doi.org/10.1134/s2079096120010096
Publikováno v:
Russian Geology and Geophysics. 59:257-267
The problem of comparison of the composition of crystalline rocks with the composition of the constituent minerals of these rocks is considered. It is proposed to present the composition of rocks and the compositions of the constituent minerals in th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c717c56a178b4987ef1f0d02e322d7fa
https://doi.org/10.1016/j.rgg.2018.03.004
https://doi.org/10.1016/j.rgg.2018.03.004
Autor:
R. G. Kuryaeva, N. V. Surkov
Publikováno v:
Journal of Materials Science. 48:4416-4426
The refractive index of Na2MgSi4O10 and Na2Al2Si4O12 glasses in the pressure range to 6.0 GPa was measured using a polarization-interference microscope and apparatus with diamond anvils. The changes in relative density, which characterize the compres
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::68fc23640e0d5b0c93b77be55daca53c
https://doi.org/10.1007/s10853-013-7260-6
https://doi.org/10.1007/s10853-013-7260-6
Autor:
R. G. Kuryaeva, N. V. Surkov
Publikováno v:
Geochemistry International. 50:1026-1031
Data on the refractive index, density, and bulk modulus variations of Di64An36 glass, which is used as a model basalt melt, were obtained with a polarization interference microscope and a high-pressure diamond anvil cell at ambient temperature and pr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5de755cd6af5425b3edcb56fb9a3681c
https://doi.org/10.1134/s0016702912120038
https://doi.org/10.1134/s0016702912120038
Autor:
Yu. G. Gartvich, N. V. Surkov
Publikováno v:
Geochemistry International. 50:799-815
The Al-rich region of the CaO-MgO-Al2O3-SiO2 system was experimentally studied at pressures of 1.0–2.8 GPa and temperatures of 1300–1535°C. The slopes of the lines of the monovariant reactions An + Sp = Cpx + Cor + (Ga) and L = Cpx + Ga + Cor +
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0aca272c09adc667839ee7b1be4ed9ff
https://doi.org/10.1134/s0016702912100060
https://doi.org/10.1134/s0016702912100060
Autor:
S. V. Kovyazin, Anatoly A. Tomilenko, A. I. Chepurov, Egor Zhimulev, V. M. Sonin, T. Yu. Timina, Aleksei Chepurov, N. V. Surkov
Publikováno v:
Russian Geology and Geophysics. 53:234-246
An experimental study of serpentine decomposition at high pressure (4.5 GPa) was carried out to elucidate if water can be preserved in the system in the form other than structural admixtures in minerals. This problem is of interest because it is wate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::62a2b8c49d6033e09cfabdd020a3befd
https://doi.org/10.1016/j.rgg.2012.02.002
https://doi.org/10.1016/j.rgg.2012.02.002
Autor:
Yu. G. Gartvich, N. V. Surkov
Publikováno v:
Russian Geology and Geophysics. 53:51-61
To elaborate physicochemical models for the origin of crystalline rocks, experimental studies of the field of high-alumina assemblages of the system CaO–MgO–Al2O3–SiO2 were carried out at 10–30 kbar and 1250–1535 °C. We have determined the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::22910e822b3c5dafe3e88ab814b5dfff
https://doi.org/10.1016/j.rgg.2011.12.004
https://doi.org/10.1016/j.rgg.2011.12.004
Autor:
Anatoly A. Tomilenko, A. I. Chepurov, Egor Zhimulev, Aleksei Chepurov, V. M. Sonin, N. V. Surkov, S. V. Kovyazin
Publikováno v:
Doklady Earth Sciences. 434:1275-1278
The subducting oceanic crust has a heterogeneous composition but mainly is composed of a mixture of anhydrous dolerite and gabbro with mafic green schist (albite + epidote + chlorite + actinolite) and amphib� olite [1]. An increase in pressure and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cd91ded58a0ebcd0bbe6d30589d36eff
https://doi.org/10.1134/s1028334x10090291
https://doi.org/10.1134/s1028334x10090291
Autor:
R. G. Kuryaeva, N. V. Surkov
Publikováno v:
Geochemistry International. 48:835-841
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d420b825d9bd642322b135d7fd73be25
https://doi.org/10.1134/s0016702910080100
https://doi.org/10.1134/s0016702910080100