Zobrazeno 1 - 10
of 52
pro vyhledávání: '"T. B. Yanovskaya"'
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 3, Iss 5, Pp 353-365 (2003)
In the framework of the linear theory, the representation theorem is derived for an incompressible liquid layer with a boundary of arbitrary shape and in a homogeneous gravity field. In addition, the asymptotic representation for the Green function,
Externí odkaz:
https://doaj.org/article/7798fd727a054d478605bc6e64bc94f9
Publikováno v:
Российский сейсмологический журнал [Russian Journal of Seismology]. 2:18-26
The radial (transversal) anisotropy of the Earth’s upper mantle was found by comparing the velocity sections of transverse waves obtained by inverse of the dispersion curves of Rayleigh and Love waves. Information on variations in anisotropy with d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2c96614a7183f62e53d8dd769025a5ac
https://doi.org/10.35540/2686-7907.2020.1.02
https://doi.org/10.35540/2686-7907.2020.1.02
Publikováno v:
Izvestiya, Physics of the Solid Earth. 55:195-204
The group velocity dispersion curves are constructed for Rayleigh and Love waves along the paths intersecting the European continent in the interval of periods from 10 to 100 s from the records of earthquakes and seismic noise. The radial anisotropy
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c204f6a957c91597f574fbff48f62f6c
https://doi.org/10.1134/s1069351319020137
https://doi.org/10.1134/s1069351319020137
Publikováno v:
Izvestiya, Physics of the Solid Earth. 54:193-200
In the problems of three-dimensional (3D) travel time seismic tomography where the data are travel times of diving waves and the starting model is a system of plane layers where the velocity is a function of depth alone, the solution turns out to str
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2d72b7c4d09d554eae97d54bf1de9415
https://doi.org/10.1134/s1069351318020167
https://doi.org/10.1134/s1069351318020167
Autor:
T. B. Yanovskaya
Publikováno v:
Izvestiya, Physics of the Solid Earth. 53:819-824
Based on the theory of surface waves in a media with weak lateral heterogeneities, an explanation is given for the peculiarities that are considered as prospecting indicators in the microseismic sounding method (MSM). According to this theory, during
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3722b4ed762633b4d036252301f9bdfe
https://doi.org/10.1134/s1069351317060076
https://doi.org/10.1134/s1069351317060076
Publikováno v:
Springer Proceedings in Earth and Environmental Sciences ISBN: 9783030217877
A new approach is proposed to study radial anisotropy of the upper mantle under the European continent. Unlike the methods used so far, we propose to interchange the order of inversion procedures. At the first stage the path-averaged velocity section
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::172586f175428f3c724b7d9e9203683e
https://doi.org/10.1007/978-3-030-21788-4_19
https://doi.org/10.1007/978-3-030-21788-4_19
Publikováno v:
Izvestiya, Physics of the Solid Earth. 52:14-28
The P-wave travel time data from the earthquakes offshore and onshore around the Black Sea are used for the tomographic reconstruction of the three-dimensional (3D) velocity distribution in the lithosphere of the region. The preliminary refinement of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1ec1ea8c3259c8c31686c3a82ed12de7
https://doi.org/10.1134/s1069351316010109
https://doi.org/10.1134/s1069351316010109
Autor:
T. B. Yanovskaya, E. L. Lyskova
Publikováno v:
Izvestiya, Physics of the Solid Earth. 49:601-609
The method for surface wave tomography based on the records of ambient seismic noise (Ambient Noise Tomography, ANT) is applied to the data from the East European and West European stations. In order to reduce the effects of the earthquakes at long p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::037ac4dfcaf9083682eddb6a2d9122a7
https://doi.org/10.1134/s1069351313040101
https://doi.org/10.1134/s1069351313040101
Autor:
T. Yu. Koroleva, T. B. Yanovskaya
Publikováno v:
Izvestiya, Physics of the Solid Earth. 48:555-561
The surface wave tomography from ambient seismic noise recorded at stations in Western Europe (WE) and on the East European Platform (EEP) revealed the structure of the crust and upper mantle in the transitional zone from the Precambrian platform to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::66dddf0dc3cdd2ad276870ee3048e2fa
https://doi.org/10.1134/s1069351312060080
https://doi.org/10.1134/s1069351312060080
Autor:
T. B. Yanovskaya
Publikováno v:
Izvestiya, Physics of the Solid Earth. 48:363-374
A method for three-dimensional (3D) ray tomography that uses the data on the travel time residuals of body waves is suggested. The underlying assumption of the method is smoothness of horizontal velocity variations. The region under study is divided
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d8430e04c4e1bd2664343a738b3bdf4b
https://doi.org/10.1134/s1069351312050059
https://doi.org/10.1134/s1069351312050059