Zobrazeno 1 - 10
of 16
pro vyhledávání: '"A. G. Goev"'
Autor:
Andrei G. Goev
Publikováno v:
Записки Горного института, Vol 266, Pp 188-198 (2024)
The article presents a study of the Earth’s crust and upper mantle in the Pechenga ore region, as well as areas adjacent to it in the northwestern part of the Kola region. Applying the receiver function technique to data acquired by three broadband
Externí odkaz:
https://doaj.org/article/2e613177b9cc42cf88df8c093a83e21d
Autor:
A. G. Goev
Publikováno v:
Moscow University Bulletin. Series 4. Geology. :88-94
A velocity section was obtained to a depth of about 250 km on the eastern margin of the Sarmatia protocraton (East-European Craton) based on P receiver functions (PRF). Seismograms of the new broadband station «Aleksandrovka» were used as initial d
Publikováno v:
Moscow University Bulletin. Series 4. Geology. :95-109
The results of natural and man- made seismicity long-term observations on the Eastern European Platform (EEP) according to the data of the small-aperture seismic group (MSG) “Mikhnevo” IDG RAS are summarized. It is shown that technogenic seismici
Autor:
A. G. Goev
Publikováno v:
Doklady Earth Sciences. 506:804-808
Publikováno v:
Doklady Earth Sciences. 504:305-309
Publikováno v:
Moscow University Geology Bulletin. 77:147-155
Publikováno v:
Moscow University Bulletin. Series 4. Geology. 1:142-149
The registration possibilities of the new broadband seismic station “Aleksandrovka” are considered. It has been established that its hardware and installation conditions make it possible to monitor the central part of the East European craton in
Publikováno v:
Doklady Earth Sciences. 501:1049-1051
Autor:
E. V. Kalinina, A. G. Goev
Publikováno v:
Doklady Earth Sciences. 494:787-789
The azimuthal elastic anisotropy of the upper mantle of the Voronezh uplift is estimated from the data of three three-component broadband stations of the Voronezh seismic network: “Storozhevoe” (VSR), “Novokhopersk” (VRH), and “Galichia Gor
Publikováno v:
Moscow University Geology Bulletin. 67:314-319
The data from the deep seismic sounding along the 2100 km long FENNOLORA profile are considered. Interpretation is made by the method of homogeneous functions with the Earth’s curvature taken into account. A seismic section of up to 200 km depth is