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pro vyhledávání: '"Olga A. Kuchay"'
Autor:
Olga A. Kuchay
Publikováno v:
Геодинамика и тектонофизика, Vol 1, Iss 3, Pp 285-296 (2015)
Earthquake concentration areas in the changeable stress-strain medium are considered. In strong earthquake centres, rupturing occurs within the limits of the arbitrarily-set boundary between deformations of positive and negative values in the field o
Externí odkaz:
https://doaj.org/article/d86d78ac8768477f9e714debddd371ea
Autor:
Olga A. Kuchay
Publikováno v:
Геодинамика и тектонофизика, Vol 3, Iss 1, Pp 59-68 (2015)
The cataclastic method developed by Yu.L. Rebetsky is applied to reconstruct the recent field of stresses related to aftershock sequences of earthquakes that occurred in the Altai-Sayan mountainous region, specifically the Altai earthquake of 27 Sept
Externí odkaz:
https://doaj.org/article/f43afd83fcbf49f0a4d63eeffe1fa8e9
Publikováno v:
Недропользование. Горное дело. Направления и технологии поиска, разведки и разработки месторождений полезных ископаемых. Экономика. Геоэкология: Материалы XVI международной конференции (20-24 апреля 2020, Новосибирск).
In the subduction zone of the Aleutian arc, the angle of inclination of the sinking Pacific plate affects the focal mechanisms of earthquakes registered in the upper part (up to 35 km) of the oceanic plate at the point of its bend, before sinking int
Autor:
Olga A. Kuchay
Publikováno v:
Geodinamika i Tektonofizika, Vol 3, Iss 1, Pp 59-68 (2015)
The cataclastic method developed by Yu.L. Rebetsky is applied to reconstruct the recent field of stresses related to aftershock sequences of earthquakes that occurred in the Altai-Sayan mountainous region, specifically the Altai earthquake of 27 Sept
Autor:
Olga A. Kuchay
Publikováno v:
Geodinamika i Tektonofizika, Vol 1, Iss 3, Pp 285-296 (2015)
Earthquake concentration areas in the changeable stress-strain medium are considered. In strong earthquake centres, rupturing occurs within the limits of the arbitrarily-set boundary between deformations of positive and negative values in the field o