The Hikurangi subduction margin, New Zealand, has not experienced any significant (> Mw
7.2) subduction interface earthquakes since historical records began∼ 170 years ago …

The segmentation of major fault systems in subduction zones controls earthquake
magnitude and location, but the causes for the existence of segment boundaries and the …

Seismic reflection profiles reveal steeply landward–dipping splay faults in the rupture area of
the magnitude (M) 8.1 Tonankai earthquake in the Nankai subduction zone. These splay …

Sea-level changes since the last glacial maximum have varied considerably from place-to-
place. This book offers a discussion of the main causes of these changes and of the …

This pattern of long and short recurrence intervals at Willapa Bay may match the pattern of
intervals between turbidity currents in Cascadia Channel, on the abyssal sea floor 200 km …

Tidal‐wetland stratigraphy reveals that great plate boundary earthquakes have caused
hundreds of kilometers of coast to subside at the Cascadia subduction zone. However …

In the center of the frontal wedge of the Hikurangi subduction zone, New Zealand, Mahia
Peninsula and its submarine continuation, Lachlan Ridge, are being uplifted and folded …

Pleistocene uplift of the Chilean coast is recorded by the formation of wave-cut platforms
resulting from marine erosion during sea-level highstands. In the Altos de Talinay area …

Spatial differences in late Quaternary structural style and deformation rates indicate a
complex pattern of strain partitioning within the transition area from oblique subduction …

Abstract Isla Santa María at the active margin of south-central Chile is the result of
earthquake-related uplift and deformation in the forearc since at least late Pleistocene time …