Geodesic
The jumps of displacements and stresses as seismic sources in Biot medium
Zapiski Nauchnykh Seminarov POMI, Mathematical problems in the theory of wave propagation. Part 26, Tome 239 (1997), pp. 164-196 
L. A. Molotkov; A. V. Bakulin. The jumps of displacements and stresses as seismic sources in Biot medium. Zapiski Nauchnykh Seminarov POMI, Mathematical problems in the theory of wave propagation. Part 26, Tome 239 (1997), pp. 164-196. http://geodesic.mathdoc.fr/item/ZNSL_1997_239_a14/
@article{ZNSL_1997_239_a14,
     author = {L. A. Molotkov and A. V. Bakulin},
     title = {The jumps of displacements and stresses as seismic sources in {Biot} medium},
     journal = {Zapiski Nauchnykh Seminarov POMI},
     pages = {164--196},
     year = {1997},
     volume = {239},
     language = {ru},
     url = {http://geodesic.mathdoc.fr/item/ZNSL_1997_239_a14/}
}
TY  - JOUR
AU  - L. A. Molotkov
AU  - A. V. Bakulin
TI  - The jumps of displacements and stresses as seismic sources in Biot medium
JO  - Zapiski Nauchnykh Seminarov POMI
PY  - 1997
SP  - 164
EP  - 196
VL  - 239
UR  - http://geodesic.mathdoc.fr/item/ZNSL_1997_239_a14/
LA  - ru
ID  - ZNSL_1997_239_a14
ER  - 
%0 Journal Article
%A L. A. Molotkov
%A A. V. Bakulin
%T The jumps of displacements and stresses as seismic sources in Biot medium
%J Zapiski Nauchnykh Seminarov POMI
%D 1997
%P 164-196
%V 239
%U http://geodesic.mathdoc.fr/item/ZNSL_1997_239_a14/
%G ru
%F ZNSL_1997_239_a14

Voir la notice du chapitre de livre provenant de la source Math-Net.Ru

For the various point sources in homogeneous isotropic Biot medium the wave fields are determined. These sources are the centers of compressions and dilatations, the jumps of displacements and stresses, and various force couples. Among these sources the elementary point sources are selected. The wave field from all other sources can be expressed by means of the field of the elementary point sources. The wave fields of the all point sources are expressed by two ways: by the integral transforms of Fourier–Bessel and Laplace and by the formulas of Stokes form.