Zobrazeno 1 - 3
of 3
pro vyhledávání: '"Bayarsaikhan Enkhee"'
Autor:
Laurent Bollinger, Yann Klinger, Steven L. Forman, Odonbaatar Chimed, Amgalan Bayasgalan, Ulziibat Munkhuu, Ganzorig Davaasuren, Tulga Dolgorsuren, Bayarsaikhan Enkhee, Demberel Sodnomsambuu
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-9 (2021)
Abstract The spatial distribution of large earthquakes in slowly deforming continental regions (SDCR) is poorly documented and, thus, has often been deemed to be random. Unlike in high strain regions, where seismic activity concentrates along major a
Externí odkaz:
https://doaj.org/article/a26f8bda9980419fb6916f49462e7cc4
Autor:
A. Bayasgalan, Bayarsaikhan Enkhee, Odonbaatar Chimed, Steven L. Forman, Yann Klinger, Demberel Sodnomsambuu, Ulziibat Munkhuu, Tulga Dolgorsuren, Ganzorig Davaasuren, Laurent Bollinger
Publikováno v:
Scientific Reports
Scientific Reports, 2021, 11, ⟨10.1038/s41598-021-97167-w⟩
Scientific Reports, Nature Publishing Group, 2021, 11, ⟨10.1038/s41598-021-97167-w⟩
Scientific Reports, Vol 11, Iss 1, Pp 1-9 (2021)
Scientific Reports, 2021, 11, ⟨10.1038/s41598-021-97167-w⟩
Scientific Reports, Nature Publishing Group, 2021, 11, ⟨10.1038/s41598-021-97167-w⟩
Scientific Reports, Vol 11, Iss 1, Pp 1-9 (2021)
The spatial distribution of large earthquakes in Slowly Deforming Continental Regions (SDCR) is poorly documented and, thus, has often been deemed to be random. Unlike in high strain regions, where seismic activity concentrates cyclically along major
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::214b90538c9c7501b451ce6270eac850
https://doi.org/10.21203/rs.3.rs-310793/v1
https://doi.org/10.21203/rs.3.rs-310793/v1
Autor:
Nyambayar Tsend-Ayush, Maksim Bano, Ulziibat Munkhuu, Antoine Schlupp, Bayarsaikhan Enkhee, Matthieu Ferry, Jean-Rémi Dujardin
Publikováno v:
Geophysical Journal International
Geophysical Journal International, Oxford University Press (OUP), 2014, ⟨10.1093/gji/ggu130⟩
Geophysical Journal International, Oxford University Press (OUP), 2014, ⟨10.1093/gji/ggu130⟩
International audience; To estimate the seismic hazard, the geometry (dip, length and orientation) and the dynamics (type of displacements and amplitude) of the faults in the area of interest need to be understood. In this paper, in addition to geomo