Short-term interaction between silent and devastating earthquakes in Mexico. [PDF]
Cruz-Atienza VM +12 more
europepmc +1 more source
Analysis of postseismic processes : afterslip, viscoelastic relaxation and aftershocks
Der Erdbebenzyklus ist in der Regel in drei Phasen unterteilt: die interseismische, die koseismische und die postseismische Phase. Der Großteil der interseismisch akkumulierten Spannung wird durch das Hauptbeben und die postseismischen Prozesse abgebaut.
openaire +1 more source
Seismic and Aseismic Fault Slip During the Initiation Phase of the 2017 M W = 6.9 Valparaíso Earthquake. [PDF]
Caballero E +5 more
europepmc +1 more source
Afterslip associated with interplate earthquakes and the viscoelastic behavior of rocks
Yusuke Kawada +3 more
openaire +2 more sources
Seismological evidence for a multifault network at the subduction interface. [PDF]
Chalumeau C +6 more
europepmc +1 more source
Seismic rhythms: Earthquake response to tectonic, hydrological, and tidal forcing in California. [PDF]
Sirorattanakul K, Avouac JP.
europepmc +1 more source
Global subduction slow slip events and associated earthquakes. [PDF]
Dascher-Cousineau K, Bürgmann R.
europepmc +1 more source
Relationship of preseismic, coseismic, and postseismic fault ruptures of two large interplate aftershocks of the 2011 Tohoku earthquake with slow-earthquake activity. [PDF]
Kubo H, Nishikawa T.
europepmc +1 more source
Dynamics of non-self-similar earthquakes illuminated by a controlled fault asperity. [PDF]
Okubo K, Yamashita F, Fukuyama E.
europepmc +1 more source
Illuminating subduction zone rheological properties in the wake of a giant earthquake. [PDF]
Weiss JR +16 more
europepmc +1 more source

