Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Yu. G. Farafonova"'
Autor:
Yu. G. Farafonova, I. M. Demina
Publikováno v:
Geomagnetism and Aeronomy. 56:415-425
The possibilities of determining arbitrary current loop parameters based on the spatial structures of the magnetic field components generated by this loop on a sphere with a specified radius have been considered with the use of models. The model para
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1d67ab4fee577931a37dde251ca2c7b4
https://doi.org/10.1134/s0016793216030038
https://doi.org/10.1134/s0016793216030038
Publikováno v:
Geomagnetism and Aeronomy. 48:812-821
The developed dynamic model of the main geomagnetic field (MGF) includes the sources of three levels, which have existed and continuously changed during the 100-year period. The spatial-temporal dynamics of the secular variations in MGF has been cons
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2e985709da7af882f9e872d6fcd4ecba
https://doi.org/10.1134/s0016793208060157
https://doi.org/10.1134/s0016793208060157
Publikováno v:
Geomagnetism and Aeronomy. 48:542-550
The effect of different-level sources on the spatial structure of the secular variations has been considered based on the dynamic model of sources of the main geomagnetic field developed by us. It has been obtained that the development of 13 most pow
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c20ed22adb6fb645f9f9c878279072cf
https://doi.org/10.1134/s0016793208040166
https://doi.org/10.1134/s0016793208040166
Upper mantle structure beneath central Western Europe from data on phase velocities of surface waves
Autor:
Yu. G. Farafonova
Publikováno v:
Izvestiya-Physics of the Solid Earth
The deep structure of the upper mantle is determined from data on phase velocities of Love and Rayleigh waves measured by a differential method on traces between two stations in central Western Europe. One-dimensional velocity structures are first co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0e07cb857746a42d97f1fe09edb03e2e
https://doi.org/10.1134/s1069351308010084
https://doi.org/10.1134/s1069351308010084
Publikováno v:
Geomagnetism and Aeronomy. 47:263-270
The dipole model of the main geomagnetic field sources has been developed by the authors for several years. At present, the model includes 13 sources that existed and continuously developed during the 20th century. It has been assumed that the main d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7aef20180c129d920f36b40751376795
https://doi.org/10.1134/s0016793207020168
https://doi.org/10.1134/s0016793207020168
Publikováno v:
Geomagnetism and Aeronomy. 46:129-138
The model of the main geomagnetic field sources, including 12 more dipoles in addition to the main dipole, is presented. The source parameters have been determined for the 100-year-long period at an interval of 5 years. The problem is solved using th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9d4fb43fd87ad6c2a87ffd5dce136054
https://doi.org/10.1134/s0016793206010142
https://doi.org/10.1134/s0016793206010142
The present-day Alpine region began to form morethan 100 Ma ago with the subduction of a Tethyanbranch beneath the Adriatic plate, eventually arriving atthe collisional stage of the European continental litho-sphere at about 40 Ma ago. Presently, Afr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::819f28bca3df50a3f06721ecb97d8df6
https://hdl.handle.net/11368/1698619
https://hdl.handle.net/11368/1698619
