A systematic compilation and characterisation of many reports of neotectonic crustal
deformation in Norway (both on local and regional scales) has identified two neotectonic …

Abstract The Nankai-Suruga Trough, the subduction zone that lies immediately south of
Japan's densely populated southern coastline, generates devastating great earthquakes …

Slip rates across active faults and folds show that late Quaternary faulting is distributed
across the central Tien Shan, not concentrated at its margins. Nearly every intermontane …

Abstract The Chi-Chi earthquake provides dramatic evidence of the damaging effects of
surface ground deformation to buildings, lifelines, and other facilities. Much of the building …

The 1999 Chi‐Chi earthquake, Mw= 7.6, broke a major thrust fault along the western
foothills of the Central Range of Taiwan. We have measured the horizontal coseismic …

Abstract The Chelungpu fault, Taiwan, ruptured in a M w 7.6 earthquake on 21 September
1999, producing a 90-km-long surface rupture. Analysis of core from two holes drilled …

Large to great earthquakes and related tsunamis generated on the Aleutian megathrust
produce major hazards for both the area of rupture and heavily populated coastlines around …

The Aleutian subduction zone is one of the most seismically active plate boundaries and the
source of several of the world's largest historic earthquakes. The structural architecture of the …

Because earthquakes on large active thrust or reverse faults are not always accompanied
with surface rupture, paleoseismological estimation of their associated seismic hazard is a …

The dextral-reverse Alpine fault is the major onshore plate-boundary structure between the
Australian and Pacific plates in New Zealand. No previous study of the central portion of the …