Characterizing the seismogenic zone of a major plate boundary subduction thrust: Hikurangi Margin, New Zealand
LM Wallace, M Reyners, U Cochran… - Geochemistry …, 2009 - Wiley Online Library
The Hikurangi subduction margin, New Zealand, has not experienced any significant (> Mw
7.2) subduction interface earthquakes since historical records began∼ 170 years ago …
7.2) subduction interface earthquakes since historical records began∼ 170 years ago …
[HTML][HTML] Geological evidence for past large earthquakes and tsunamis along the Hikurangi subduction margin, New Zealand
Abstract The Hikurangi subduction margin, New Zealand, has not produced large
subduction earthquakes within the short written historic period (~ 180 years) and the …
subduction earthquakes within the short written historic period (~ 180 years) and the …
[HTML][HTML] Subduction zone megathrust earthquakes
Subduction zone megathrust faults host Earth's largest earthquakes, along with multitudes of
smaller events that contribute to plate convergence. An understanding of the faulting …
smaller events that contribute to plate convergence. An understanding of the faulting …
Three-dimensional splay fault geometry and implications for tsunami generation
Megasplay faults, very long thrust faults that rise from the subduction plate boundary
megathrust and intersect the sea floor at the landward edge of the accretionary prism, are …
megathrust and intersect the sea floor at the landward edge of the accretionary prism, are …
Interseismic coupling and seismic potential along the Central Andes subduction zone
We use about two decades of geodetic measurements to characterize interseismic strain
build up along the Central Andes subduction zone from Lima, Peru, to Antofagasta, Chile …
build up along the Central Andes subduction zone from Lima, Peru, to Antofagasta, Chile …
Tearing and breaking off of subducted slabs as the result of collision of the Panama Arc‐Indenter with northwestern South America
We present two regional, lithospheric cross sections that illustrate eastward‐and
southeastward‐dipping, subducted slabs to depths of 315 km beneath the surface of …
southeastward‐dipping, subducted slabs to depths of 315 km beneath the surface of …
Forearc basins: Types, geometries, and relationships to subduction zone dynamics
A Noda - Bulletin, 2016 - pubs.geoscienceworld.org
Forearc basins are one of the fundamental sedimentary basins, and they preserve various
geological phenomena arising from dynamic interactions between subducting and …
geological phenomena arising from dynamic interactions between subducting and …
Segmentation of megathrust rupture zones from fore‐arc deformation patterns over hundreds to millions of years, Arauco peninsula, Chile
This work explores the control of fore‐arc structure on segmentation of megathrust
earthquake ruptures using coastal geomorphic markers. The Arauco‐Nahuelbuta region at …
earthquake ruptures using coastal geomorphic markers. The Arauco‐Nahuelbuta region at …
Relationship between bend‐faulting at trenches and intermediate‐depth seismicity
CR Ranero, A Villaseñor… - Geochemistry …, 2005 - Wiley Online Library
We have studied faulting associated with bending of the incoming oceanic plate along
segments of Middle America and Chile subduction zones and its relationship to intermediate …
segments of Middle America and Chile subduction zones and its relationship to intermediate …
A new view for the geodynamics of Ecuador: Implication in seismogenic source definition and seismic hazard assessment
A new view of Ecuador's complex geodynamics has been developed in the course of
modeling seismic source zones for probabilistic seismic hazard analysis. This study focuses …
modeling seismic source zones for probabilistic seismic hazard analysis. This study focuses …