Fault identification plays a vital role in geologic structure interpretation, reservoir
characterization, and reservoir evaluation. The traditional process for fault identification is …

Abstract The Alpine Fault is an oblique strike‐slip fault that is known to fail in large
magnitude (M7–8) earthquakes, yet it is currently seismically quiescent. We examine the low …

We reveal the subsurface bedrock topography and sedimentary succession of one of the
deepest glacially-formed basins in the Eastern Alps: the Lienz Basin in the Upper Drau …

Using bathymetry and ROV dives, we investigate two successive flip‐flop detachment faults
(D1 active, D2 older) in the near‐amagmatic 64° 35′ E region of the SWIR. Kilometer‐sized …

Abstract The Alpine Fault, a transpressional plate boundary between the Australian and
Pacific plates, is known to rupture quasiperiodically with large magnitude earthquakes (M …

Abstract New Zealand's Alpine Fault is a large, plate-bounding strike-slip fault, which
ruptures in large (M w> 8) earthquakes. We conducted field and laboratory analyses of fault …

Lithosphere–asthenosphere boundary (LAB) properties beneath the South Island of New
Zealand have been imaged by Sp receiver function common-conversion point stacking. In …

Seismically detected low‐velocity zones are commonly associated with major crustal faults.
In order to accurately interpret these low‐velocity zones and understand processes that …

Abstract The transpressional Alpine Fault in New Zealand has created a thick shear zone
with associated highly anisotropic rocks. Low seismic velocity zones and high seismic …

Active traces of the reverse dextral Alpine Fault were poorly located on the true left
(southwest) side of the Whataroa River. Mapping using airborne LiDAR-derived high …