Zobrazeno 1 - 5
of 5
pro vyhledávání: '"A. O. Verpakhovskaya"'
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
Publikováno v:
Geofizicheskiy Zhurnal; Том 37, № 3 (2015); 50-65
Геофизический журнал; Том 37, № 3 (2015); 50-65
Геофізичний журнал; Том 37, № 3 (2015); 50-65
Геофизический журнал; Том 37, № 3 (2015); 50-65
Геофізичний журнал; Том 37, № 3 (2015); 50-65
The method of 3D finite-difference migration of the field of refracted waves is proposed, which takes into account their penetration into refracting strata. Theoretical grounds and special features of the method of finite-difference deep migration of
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
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
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