Zobrazeno 1 - 10
of 45
pro vyhledávání: '"V.N. Pilipenko"'
Autor:
K.G. Kondrashin, V.N. Pilipenko
Publikováno v:
Engineering and Construction Bulletin of the Caspian Region. 112:20-25
In the practice of construction on loess and loess soils, there are numerous cases of significant and uneven settlement of the foundations of buildings and structures due to the ability of subsidence soils to significantly decrease in volume (compact
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3392f0b3ddd8b1b75c5475fed361879c
https://doi.org/10.52684/2312-3702-2021-36-2-20-25
https://doi.org/10.52684/2312-3702-2021-36-2-20-25
Autor:
A.O. Verpakhovskaya, V.N. Pilipenko
Publikováno v:
Geofizicheskiy Zhurnal. 42:176-191
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::df318f24f4570c7a798ec69634ec2275
https://doi.org/10.24028/gzh.0203-3100.v42i6.2020.222293
https://doi.org/10.24028/gzh.0203-3100.v42i6.2020.222293
Autor:
A.O. Verpakhovskaya, V.N. Pilipenko
Publikováno v:
Geofizicheskiy Zhurnal. 41:3-26
Three-dimensional modeling of temporal field allows reconstructing the kinamatics of wave processes observed in the Earth during seismic studies and determine in such a way spatial position into it of the studied objects. Modeling is also an importan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d92eb8e9e6da56ffe4bd2e904cd6aecf
https://doi.org/10.24028/gzh.0203-3100.v41i5.2019.183636
https://doi.org/10.24028/gzh.0203-3100.v41i5.2019.183636
Autor:
V.N. Pilipenko, A. O. Verpakhovskaya
Publikováno v:
Geofizicheskiy Zhurnal. 40:52-67
Seismic migration allows solving different problems of seismic exploration and depending on the properties of the wave field which take part during the processing is subdivided into two types: kinematic and dynamic. Kinematic migration allows to dete
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4983d01b9e3515e1502f805af7efd0a8
https://doi.org/10.24028/gzh.0203-3100.v40i6.2018.151007
https://doi.org/10.24028/gzh.0203-3100.v40i6.2018.151007
Publikováno v:
Geofizicheskiy Zhurnal; Том 38, № 1 (2016); 43-56
Геофизический журнал; Том 38, № 1 (2016); 43-56
Геофізичний журнал; Том 38, № 1 (2016); 43-56
Геофизический журнал; Том 38, № 1 (2016); 43-56
Геофізичний журнал; Том 38, № 1 (2016); 43-56
Migration methods are traditionally subdivided into two groups depending on carrying out the procedure of summing up the route by the method of common deep point (CDP): before and after summing up (pre- and post-stack migration in English variant). D
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a3a5eb97597f78ea868cc8958c0ffdd3
http://journals.uran.ua/geofizicheskiy/article/view/107721
http://journals.uran.ua/geofizicheskiy/article/view/107721
Publikováno v:
Izvestiya, Physics of the Solid Earth. 46:943-954
The main results of deep seismic sounding (DSS) are usually presented in the form of high-velocity models of the medium. Some model examples and the international DOBRE profile have shown that the informativeness of the data obtained can be significa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c73842629caf5f4f417cd7c806fdf394
https://doi.org/10.1134/s1069351310110042
https://doi.org/10.1134/s1069351310110042
Publikováno v:
Tectonophysics. 308:445-457
The 440 km long POLAR profile runs approximately SW to NE across the Baltic Shield from the Karelian Province through the Lapland Granulite Belt and the Kola Peninsula Province in northern Finland and northern Norway. The migration method developed b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bb7b5c9a609a40f8d93188cfaccb72e5
https://doi.org/10.1016/s0040-1951(99)00144-4
https://doi.org/10.1016/s0040-1951(99)00144-4
Publikováno v:
Geofizicheskiy Zhurnal; Том 34, № 3 (2012); 40-48
Геофизический журнал; Том 34, № 3 (2012); 40-48
Геофізичний журнал; Том 34, № 3 (2012); 40-48
Геофизический журнал; Том 34, № 3 (2012); 40-48
Геофізичний журнал; Том 34, № 3 (2012); 40-48
The final procedure of the standard production processing and interpretation of seismic data is the post-stack migration by the central deep point method (CDP). However, in practice, a more informative image of the deep section is given by the pre-st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::726d491555946660ec4e3bcdb922afa6
http://journals.uran.ua/geofizicheskiy/article/view/116636
http://journals.uran.ua/geofizicheskiy/article/view/116636
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