Zobrazeno 1 - 10
of 23
pro vyhledávání: '"A.K. Pevnev"'
Autor:
A.K. Pevnev
Publikováno v:
Геология и геофизика Юга России.
The article reasonably shows that the uppermost layer of the Earth's crust up to 25 kilometers is seismogenic. Aim. The article provides the evidence that crustal seismicity is generated not by regional stress fields of a homogeneous shear, as it was
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f641f68f8288d5c2262d68c95ba04b51
https://doi.org/10.46698/vnc.2021.53.34.009
https://doi.org/10.46698/vnc.2021.53.34.009
Autor:
A.K. Pevnev
Publikováno v:
Geodesy and Cartography. 902:48-54
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5118ef88d481af02638bb13afdf3070f
https://doi.org/10.22389/0016-7126-2015-902-8-48-54
https://doi.org/10.22389/0016-7126-2015-902-8-48-54
Autor:
A.k. Pevnev
Publikováno v:
Tectonophysics. 202:97-100
The preparation of strong crustal earthquakes is followed by elastic deformation of rocks in their definite volume (source of future earthquake) in seismogenic stratum of the Earth. The land surface, which is the upper boundary of this seismogenic la
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0c3e5e58b8568ed8096afb2cf3bc8bbb
https://doi.org/10.1016/0040-1951(92)90085-k
https://doi.org/10.1016/0040-1951(92)90085-k
Akademický článek
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Akademický článek
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Publikováno v:
Tectonophysics. 52:203-209
The Garm polygon is confined to the junction between Tien-Shan and the Peter the Great fault zone separating the Pamirs and Tien-Shan. It is just in the zone of contact between the fault zone itself and Tien-Shan (the spurs of the Gissar ridge) that
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::95053bbea6ec0304332452e8beb9e6cf
https://doi.org/10.1016/0040-1951(79)90226-9
https://doi.org/10.1016/0040-1951(79)90226-9
Publikováno v:
Studia Geophysica et Geodaetica. 22:298-303
Рaссмоmрены зaкономерносmu орuзонmaльных u верmuкaльных смещенuŭ эемноŭ nоверхносmu нa Гaрмском ео¶rt;uнaмuческом nолu оне, рaсnоложенном в зоне со
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a6e932bae6d9b268d8d7152d75f21cac
https://doi.org/10.1007/bf01627907
https://doi.org/10.1007/bf01627907
Publikováno v:
Tectonophysics. 29:429-438
The mean velocity of horizontal displacements at one of the sections of the Garm polygon over a period of more than 20 years ranged from 15 to 20 mm/year. The displacement direction is a sub-meridional rapprochement of points located at the opposite
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fa8cfe37f14a03388ceac9d41ba4462e
https://doi.org/10.1016/0040-1951(75)90171-7
https://doi.org/10.1016/0040-1951(75)90171-7
Publikováno v:
Tectonophysics. 14:183-188
On the Garm (the Pamirs) and the Alma-Ata polygons for the study of recent crustal movements anomalous deformations of the earth surface have been revealed which coincide in time with the processes of preparation and the moments of occurrence of stro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c40c0a49485cf24e3e3fc79fabcb1d56
https://doi.org/10.1016/0040-1951(72)90067-4
https://doi.org/10.1016/0040-1951(72)90067-4
Publikováno v:
Physics of the Earth and Planetary Interiors. 6:235-240
Slow tectonic deformations of the Earth's crust and the associated stresses give rise to faulting and earthquakes. A correlation between earthquakes and slow recent deformations may be observed by geophysical and geodetic methods for short periods of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cd0bf7bf18bfa3465a574317700c2ec4
https://doi.org/10.1016/0031-9201(72)90006-4
https://doi.org/10.1016/0031-9201(72)90006-4