Invited review paper: Fault creep caused by subduction of rough seafloor relief
Among the wide range of thermal, petrologic, hydrological, and structural factors that
potentially affect subduction earthquakes, the roughness of the subducting seafloor is …
potentially affect subduction earthquakes, the roughness of the subducting seafloor is …
Invited review paper: Some outstanding issues in the study of great megathrust earthquakes—The Cascadia example
Because of a combination of new observational tools and a flurry of large megathrust
earthquakes, tremendous progress has been made in recent years towards understanding …
earthquakes, tremendous progress has been made in recent years towards understanding …
Depth‐varying rupture properties of subduction zone megathrust faults
Subduction zone plate boundary megathrust faults accommodate relative plate motions with
spatially varying sliding behavior. The 2004 Sumatra‐Andaman (Mw 9.2), 2010 Chile (Mw …
spatially varying sliding behavior. The 2004 Sumatra‐Andaman (Mw 9.2), 2010 Chile (Mw …
Viscoelastic relaxation following subduction earthquakes and its effects on afterslip determination
Afterslip is commonly thought to be the controlling process in postseismic deformation
immediately following a great megathrust earthquake and is usually inferred from geodetic …
immediately following a great megathrust earthquake and is usually inferred from geodetic …
Thermal structure and megathrust seismogenic potential of the Makran subduction zone
The Makran subduction zone experienced a tsunamigenic Mw 8.1 earthquake in 1945 and
recent, smaller earthquakes also suggest seismicity on the megathrust; however, its …
recent, smaller earthquakes also suggest seismicity on the megathrust; however, its …
Heterogeneous rupture in the great Cascadia earthquake of 1700 inferred from coastal subsidence estimates
Past earthquake rupture models used to explain paleoseismic estimates of coastal
subsidence during the great AD 1700 Cascadia earthquake have assumed a uniform slip …
subsidence during the great AD 1700 Cascadia earthquake have assumed a uniform slip …
Interplate coupling model off the southwestern coast of Java, Indonesia, based on continuous GPS data in 2008–2010
We present an interplate coupling model of the Australia–Java plate interface off the
southwestern coast of Java, Indonesia, based on data from the Indonesian Permanent GPS …
southwestern coast of Java, Indonesia, based on data from the Indonesian Permanent GPS …
Contributions of poroelastic rebound and a weak volcanic arc to the postseismic deformation of the 2011 Tohoku earthquake
A better understanding of fluid-related processes such as poroelastic rebound of the upper
crust and weakening of the lower crust beneath the volcanic arc helps better understand and …
crust and weakening of the lower crust beneath the volcanic arc helps better understand and …
Systematic characterization of morphotectonic variability along the Cascadia convergent margin: Implications for shallow megathrust behavior and tsunami hazards
JT Watt, DS Brothers - Geosphere, 2021 - pubs.geoscienceworld.org
Studies of recent destructive megathrust earthquakes and tsunamis along subduction
margins in Japan, Sumatra, and Chile have linked forearc morphology and structure to …
margins in Japan, Sumatra, and Chile have linked forearc morphology and structure to …
Subducted seamounts and recent earthquakes beneath the central Cascadia forearc
AM Tréhu, RJ Blakely, MC Williams - Geology, 2012 - pubs.geoscienceworld.org
Bathymetry and magnetic anomalies indicate that a seamount on the Juan de Fuca plate
has been subducted beneath the central Cascadia accretionary complex and is now …
has been subducted beneath the central Cascadia accretionary complex and is now …