Zobrazeno 1 - 10
of 57
pro vyhledávání: '"V. A. Kronrod"'
Autor:
V. A. Dorofeeva, A. N. Dunaeva, S. I. Ipatov, V. A. Kronrod, E. V. Kronrod, O. L. Kuskov, M. Ya. Marov, A. V. Rusol
Publikováno v:
Advances in Geochemistry, Analytical Chemistry, and Planetary Sciences ISBN: 9783031098826
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d29fad2676f301363c45de00d049e613
https://doi.org/10.1007/978-3-031-09883-3_14
https://doi.org/10.1007/978-3-031-09883-3_14
Publikováno v:
Geochemistry International. 59:1018-1037
Abstract One of the pivoting problems of the geochemistry and geophysics of the Moon is the structure of its central region, i.e., its core and adjacent transition layer located at the boundary between the solid mantle and liquid or partially molten
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::95ef40395a92f8947d2d28e7cbafad47
https://doi.org/10.1134/s0016702921110069
https://doi.org/10.1134/s0016702921110069
Publikováno v:
Геохимия. 64:567-584
Based on the joint inversion of seismic and gravity data in combination with the Gibbs free energy minimization method for calculating phase equilibria in the framework of the Na 2 O-TiO 2 -CaO-FeO-MgO-Al 2 O 3 -SiO 2 system, the influence of the the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::34f3a867f1f22bddb97238eb3db3a17b
https://doi.org/10.31857/s0016-7525646567-584
https://doi.org/10.31857/s0016-7525646567-584
Publikováno v:
Geochemistry International. 57:605-620
Based on the joint inversion of seismic and gravity data in combination with phase equilibrium calculations within the Na2O–TiO2–CaO–FeO–MgO–Al2O3–SiO2 system using the method of Gibbs free energy minimization, we estimated the influence
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a48862d877bc4acd5ef142e6f23142db
https://doi.org/10.1134/s0016702919060041
https://doi.org/10.1134/s0016702919060041
Publikováno v:
Solar System Research. 53:75-90
Internally consistent models of the thermal state, chemical composition and mineralogy of the three-layer mantle of the Moon are constructed based on the joint inversion of gravity, seismic and petrological-geochemical data within the Na2O-TiO2-CaO-F
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::75c09c634228e5dc08ee530a8b644622
https://doi.org/10.1134/s0038094619010040
https://doi.org/10.1134/s0038094619010040
Publikováno v:
Physics of the Earth and Planetary Interiors. 286:1-12
The main purpose of the present study is to evaluate the lunar bulk composition (BSM) and the composition of a three-layer mantle based on a joint inversion of lunar mass and moment of inertia, and the mantle seismic velocity profiles in combination
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dba3ee151c46b8a33a606a238ab3a16f
https://doi.org/10.1016/j.pepi.2018.10.011
https://doi.org/10.1016/j.pepi.2018.10.011
Publikováno v:
Uchenye Zapiski Kazanskogo Universiteta. Seriya Fiziko-Matematicheskie Nauki. 161:24-38
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::61209abc0ae9de7ccbd6b6e2583a34bc
https://doi.org/10.26907/2541-7746.2019.1.24-38
https://doi.org/10.26907/2541-7746.2019.1.24-38
Publikováno v:
Doklady Earth Sciences. 483:1475-1479
The bulk composition of the silicate Moon (crust + mantle, BSM) is determined on the basis of inversion of gravitational and seismic data. It is shown that the mantle refractory oxides form two different groups depending on the thermal state. By the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::95bcb4f004ee0fd4db7abb4a26a7e677
https://doi.org/10.1134/s1028334x18110211
https://doi.org/10.1134/s1028334x18110211
Publikováno v:
Доклады академии наук. 483:319-324
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2972a556fad046bfd9861d157007da38
https://doi.org/10.31857/s086956520003257-5
https://doi.org/10.31857/s086956520003257-5
Publikováno v:
Solar System Research. 52:467-479
The variations of the bulk composition of the silicate Moon (crust + mantle = Bulk Silicate Moon, BSM) depending on the thermal state are explored based on the joint inversion of gravitational, seismic, and petrologic data within the Na2O–TiO2–Ca
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::69016855e53004053c2ee0f43775dab1
https://doi.org/10.1134/s0038094618060047
https://doi.org/10.1134/s0038094618060047