Zobrazeno 1 - 10
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pro vyhledávání: '"Seismogenic layer"'
Akademický článek
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Publikováno v:
Surveys in Geophysics. 42:1143-1170
We consider the thermal state of the lithosphere in the poorly studied region, including the NE flank of the Baikal rift zone and its adjacent areas (110°–122° E, 50°–63° N). For this purpose, spectral analysis of the EMAG2v3 lithospheric geo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5b68c4b13191fd27dfecfa6f59367021
https://doi.org/10.1007/s10712-021-09651-7
https://doi.org/10.1007/s10712-021-09651-7
Autor:
Emir Balkan, Bülent Oruç
Publikováno v:
Acta Geophysica. 69:1137-1149
The strong earthquake with magnitude 6.9 occurred offshore at the northernmost edge of the Samos Island and was strongly felt in the north Aegean islands and Izmir metropolitan city. In this study, the effective elastic thicknesses of the lithosphere
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8732171e57017bb7c8a876c75f74030b
https://doi.org/10.1007/s11600-021-00604-7
https://doi.org/10.1007/s11600-021-00604-7
Autor:
Yong-Seok Jang, Chang-Whan Oh
Publikováno v:
Geosciences Journal. 25:59-70
The southwestern Gyeonggi Massif features many faults. The main faults are NE-striking faults, including the Jeonju and Kwangju faults, and they are cut by N-S- and NNE-striking faults. Additionally, E-W-, WNW-, and NW-striking faults occur as minor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cfafb84f2ef022bc4d3682fdec533243
https://doi.org/10.1007/s12303-020-0049-0
https://doi.org/10.1007/s12303-020-0049-0
Autor:
A. A. Lukk, V. G. Leonova
Publikováno v:
Izvestiya, Atmospheric and Oceanic Physics. 56:657-677
An example of seven seismogenic regions of the world with different conditions of tectonic deformation confirms the reliability of confinedness of weak earthquakes to two horizons in the Earth’s continental crust at depths of 5 and 10 km, regardles
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b3540df755243ede0bfae4d07213d90b
https://doi.org/10.1134/s0001433820070063
https://doi.org/10.1134/s0001433820070063
Akademický článek
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Publikováno v:
Frontiers of Earth Science. 14:647-659
The Linfen rift is a Cenozoic extensional rift with significant seismicity and seismic hazards. Studies of this rift shed light on deep dynamic processes and seismogenic mechanisms relevant to crustal structure and seismic activity. We first conducte
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::36861906ee035dc579b0f2fc175a7bdd
https://doi.org/10.1007/s11707-019-0804-6
https://doi.org/10.1007/s11707-019-0804-6
Publikováno v:
Pure and Applied Geophysics. 177:1725-1738
The Gulf of Cadiz has been affected by a long and complex geodynamic evolution. The lithospheric structure is poorly understood in this region, and it also shows a diffuse seismicity, spanning over a broad area. The Canary Archipelago has been extens
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::63a4498164324bbbd5a5419bc6002c1c
https://doi.org/10.1007/s00024-019-02380-4
https://doi.org/10.1007/s00024-019-02380-4
Autor:
Hiroyuki Noda, Yuki Miyake
Publikováno v:
Earth, Planets and Space, Vol 71, Iss 1, Pp 1-12 (2019)
Along subduction interfaces or some major faults, a seismogenic layer in the upper crust is underlain by a zone of slow-slip events (SSEs) and tremors, and seismicity disappears at greater depths. The transition between seismogenic and aseismic behav
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::01c9c272b8111e99f35ef49906f82fed
https://doaj.org/article/45f95b48b9ff4c8fafbe391f16bba9e1
https://doaj.org/article/45f95b48b9ff4c8fafbe391f16bba9e1
Autor:
Marie Violay, Damien Deldicque, Francois Passelegue, Giulio Di Toro, J. A. Tielke, Julian Mecklenburgh
Pseudotachylytes are fine‐grained fault rocks that solidify from melt that is produced in fault zones during earthquakes. Exposed sections of natural fault zones reveal evidence of post‐seismic plastic deformation (i.e. reactivation) of pseudotac
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::aadec278f932048190d5ee1f6ed5cc4c
http://hdl.handle.net/11577/3400839
http://hdl.handle.net/11577/3400839
