Zobrazeno 1 - 10
of 63
pro vyhledávání: '"Matt J. Ikari"'
Autor:
Matt J. Ikari, Marianne Conin
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 25, Iss 9, Pp n/a-n/a (2024)
Abstract The slip behavior of crustal faults is known to be controlled by the composition of the fault gouge, but the exact mechanisms, especially considering the role of water‐rock interactions, are still under investigation. Here, we use a geoche
Externí odkaz:
https://doaj.org/article/58af5ab92fea4bd79b8718b3576717ce
Autor:
Matt J. Ikari, Philipp Haberkorn
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 10, Pp n/a-n/a (2023)
Abstract Frictional slip instability, resulting in intermittent “stick‐slip” rather than continuous sliding, is a phenomenon that depends on the frictional properties of the sliding area and the stiffness of the surrounding material. For geomec
Externí odkaz:
https://doaj.org/article/dc5ea011d63f4274be50b9141d047eb4
Publikováno v:
Earth, Planets and Space, Vol 74, Iss 1, Pp 1-15 (2022)
Abstract The Nankai Trough megasplay fault hosts diverse modes of fault slip, ranging from slow slip events to megathrust earthquakes, and is responsible for related phenomena such as tsunamis and submarine landslides. All types of slip events requir
Externí odkaz:
https://doaj.org/article/cd33825d988043bb81b3efc3c0c66dcc
Autor:
Genevieve L. Coffey, Heather M. Savage, Pratigya J. Polissar, Francesca Meneghini, Matt J. Ikari, Åke Fagereng, Julia K. Morgan, Maomao Wang
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 8, Pp n/a-n/a (2021)
Abstract The Hikurangi subduction zone is capable of producing moderate to large earthquakes as well as regularly repeating slow slip events. However, it is unclear what structures host these different slip styles along the margin. Here we address wh
Externí odkaz:
https://doaj.org/article/9b7dd37af7d344459aa0f502eed9bd57
Autor:
Matt J. Ikari, Laura M. Wallace, Hannah S. Rabinowitz, Heather M. Savage, Ian J. Hamling, Achim J. Kopf
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 21, Iss 2, Pp n/a-n/a (2020)
Abstract Slow slip events (SSEs) are recognized as an important component of plate boundary fault slip, and there is a need for laboratory friction data on natural samples to guide comparisons with natural SSEs. Here, we compile a comprehensive catal
Externí odkaz:
https://doaj.org/article/b5e718fc65e243ada399f24a76377257
Laboratory measurements can determine the potential for geologic materials to generate unstable (seismic) slip, but a direct relation between sliding behavior in the laboratory and physical characteristics observable in the field is lacking, especial
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0e4f5e1add0524db6107e453d6eb1119
http://hdl.handle.net/10852/99962
http://hdl.handle.net/10852/99962
Autor:
Hanaya Okuda, Achim J Kopf, Katja Stanislowski, Alexander Roesner, Andre Hüpers, Matt J. Ikari, Asuka Yamaguchi
Publikováno v:
Journal of Geophysical Research: Solid Earth. 126
Autor:
Matt J. Ikari, Srisharan Shreedharan, Chris Marone, Clay Wood, Demian M. Saffer, Laura M. Wallace
Slow slip events (SSEs) have been identified at subduction zones globally as an important link in the continuum between elastodynamic ruptures and stable creep. The northern Hikurangi margin is hom...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b65a85ac99b25d04f4e8769f2bfb6b5e
https://doi.org/10.1002/essoar.10507803.1
https://doi.org/10.1002/essoar.10507803.1
Publikováno v:
Oceanography. 32:106-118
Publikováno v:
Pure and Applied Geophysics. 176:3951-3973
The generation of the 2011 Tohoku-oki earthquake has been modeled by many authors by considering a dynamic weakening mechanism such as thermal pressurization (TP). Because the effects of TP on afterslip have not been investigated, this study develops