Zobrazeno 1 - 8
of 8
pro vyhledávání: '"неприливные вариации силы тяжести"'
Autor:
Yu. V. Antonov, I. A. Ponomarenko
Publikováno v:
Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 4, Pp 78-84 (2019)
Gravimetric and seismic pulsations coincide in time with each other. This synchrony circumstance was previously analyzed for the Eurasian continent, where the data on seismic and gravimetric observations are available. The pulsations of the gravimetr
Externí odkaz:
https://doaj.org/article/59e368fdf81246399f66f5174aef95cf
Autor:
Yu. V. Antonov, I. Yu. Antonova
Publikováno v:
Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 1, Pp 60-66 (2019)
For the first time, gravity pulsations were detected during the processing of stationary observations at the Geodynamic range of RAS in Bishkek (2014). Then, similar surges were detected in stationary seismic observations in the city of Voronezh, whi
Externí odkaz:
https://doaj.org/article/44f33773bb37420f9940ed854406dacc
Autor:
Yu. V. Antonov
Publikováno v:
Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 3, Pp 51-57 (2018)
A possible correlation between the destructive earthquakes of magnitude M = 7 and above and luni-solar gravity variations between 1975 and 2015 has been analyzed. The lunar-solar variations are characterized by three extreme points: the maximum and m
Externí odkaz:
https://doaj.org/article/bed9f4040a884348975f5df0c780f4e2
Autor:
Yu. V. Antonov
Publikováno v:
Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 4, Pp 66-71 (2017)
Non-tidal variations of gravity are the residual part of the monitoring of the variations after subtraction from them the lunar-solar gravity variations and the drift of the zero point of the gravimeter. Non-tidal variations have a complex morphology
Externí odkaz:
https://doaj.org/article/46987f25fc93443e9bf425236ccd7d27
Autor:
YU. V. Antonov
Publikováno v:
Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 2, Pp 70-76 (2017)
Non-tidal variations of gravity are the residual part of the monitoring of the variations after subtraction from them the lunar-solar gravity variations and the drift of the zero point of the gravimeter. Non-tidal variations are sometimes of complex
Externí odkaz:
https://doaj.org/article/9524ce428ce64b139fd4fab448a9555b
Publikováno v:
Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 2, Pp 39-43 (2016)
The joint change in variations of magnetotelluric field of the Earth and un-tidal variations of gravity, registered at the territory of Bishkek Geodynamic Polygon, are considered. There is a clear relationship of these variations. During the pulsatio
Externí odkaz:
https://doaj.org/article/fb320426d781481ab1eb9a033882c760
Autor:
Y. U. Antonov, I. A. Sizask
Publikováno v:
Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 5, Pp 46-52 (2015)
The results of simultaneous observations of the vertical component of the seismic field in Voronezh (Russia) and non-tidal variations of gravity in Bishkek (Kyrgyzstan) are considered in the paper. Pulsations are observed in gravity and seismic field
Externí odkaz:
https://doaj.org/article/8a87de857e7742e8952f0b52088e6eea
Publikováno v:
Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 3, Pp 59-63 (2015)
The joint change variations of magnetotelluric field of the Earth and un-tidal variations of gravity, registered on the territory of Bishkek Geodynamic Polygon, are considered. There is a clear relationship of these variations. Obviously, a joint ana
Externí odkaz:
https://doaj.org/article/3b89bb77878b439eb42c5857a8aef6f4