Zobrazeno 1 - 10
of 12
pro vyhledávání: '"L. P. Nasonova"'
Publikováno v:
Solar System Research. 54:295-306
The possible distribution of density and stress anomalies in the interior of the Moon is determined. For this purpose, we have developed a new solution of the incorrect inverse gravimetry problem developed by the authors, tested for the Earth and Mar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d022b7f0c52dc4eade3e48b8080e6a3b
https://doi.org/10.1134/s0038094620040048
https://doi.org/10.1134/s0038094620040048
Publikováno v:
Journal of Geophysical Research: Space Physics. 122:77-88
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7e940b34e752f64f6f5e2d14c74fa994
https://doi.org/10.1002/2016ja022623
https://doi.org/10.1002/2016ja022623
Publikováno v:
Izvestiya, Physics of the Solid Earth. 50:427-443
The formulas that allow, within the quadratic approximation, for the contribution of the anomalous masses, distributed along the height relative to the reference ellipsoid, in the Stokes parameters are derived. It is shown that the contribution of th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c555b3cde8d3949b680c5a6f8b567bad
https://doi.org/10.1134/s106935131403001x
https://doi.org/10.1134/s106935131403001x
Publikováno v:
Moscow University Physics Bulletin. 67:218-225
We determined the possible compensation depths for relief harmonics of different degrees and orders. The relief is shown to be completely compensated within the depth range of 0 to 1400 km. The lateral distributions of compensation masses are determi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8c258deee40bc71293c86a811a032abb
https://doi.org/10.3103/s0027134912020075
https://doi.org/10.3103/s0027134912020075
Publikováno v:
Moscow University Physics Bulletin. 66:64-71
This study determined the contribution of Martian topography and the density jump at the Mohorovicic discontinuity (M) to the gravity in a quadratic approximation. It also resolved the problem of determining the possible depths of compensation for to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::49685a6ab5990203a5b83f1a48ceddd1
https://doi.org/10.3103/s0027134911010085
https://doi.org/10.3103/s0027134911010085
Autor:
N. A. Chuikova, L. P. Nasonova
Publikováno v:
Moscow University Physics Bulletin. 62:397-405
Formulas that include the contribution from dipole-distributed anomalous masses represented as layers distributed in height relative to the reference ellipsoid to the gravitational field in the quadratic approximation have been derived. The relations
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::da6a5954f38e57f1169588a5727f3de4
https://doi.org/10.3103/s0027134907060148
https://doi.org/10.3103/s0027134907060148
Publikováno v:
Astronomical & Astrophysical Transactions. 26:391-399
The contribution to the Earth external and internal gravity field from isostatically equilibrated masses of relief, density jumps on Moho boundary and anomalous masses of crust and upper mantle of the Earth in linear and quadratic approximation is fo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a9041e94041b17cf0a427d3719fa301f
https://doi.org/10.1080/10556790701594999
https://doi.org/10.1080/10556790701594999
Autor:
L. P. Nasonova, N.A. Chujkova
Publikováno v:
Astronomical & Astrophysical Transactions. 26:361-369
The explicit form for the quadratic contribution to the gravitational field from the dipole distributed anomalous masses is found. The anomalous masses are represented in the form of layers of variable height, arranged relative to the reference ellip
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::596d439efd60d62e4d6128945d41a571
https://doi.org/10.1080/10556790701592134
https://doi.org/10.1080/10556790701592134
Publikováno v:
International Association of Geodesy Symposia ISBN: 9783319398198
The original method for solving the inverse incorrect problem of gravimetry is developed. The method allows to find the anomalous density structure of terrestrial planets from space-based observations of the gravity field and topography. Previously w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ecbce0ab94198e2946020f7511b54b78
https://doi.org/10.1007/1345_2015_195
https://doi.org/10.1007/1345_2015_195
Publikováno v:
Astronomical & Astrophysical Transactions. 22:519-523
A criterion on the stability of motion due to Hill in the problem of many absolutely rigid bodies possessing an arbitrary form and structure of the density distribution is established. A graphical illustration of the results obtained is given for the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8864780e7439477b4e71d90f8fab01f8
https://doi.org/10.1080/1055679031000139433
https://doi.org/10.1080/1055679031000139433