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Publications tagged with [fault rupture]

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<p>Analysis of light detection and ranging (lidar) derived topography combined with field data enables measurement of small (&lt;30 m), previously unrecognized dextral offsets beneath dense temperate rainforest along New Zealand&rsquo;s central Alpine fault. ...
Reference: GEOLOGY, May 2014; v. 42; no. 5; p. 411–414
<p>The 2011 rupture of previously undetected blind faults beneath Christchurch, New Zealand, in moment magnitude (Mw) 6.2 and 6.0 earthquakes triggered major rockfalls that caused fatalities and infrastructure damage. Here we use field, geospatial, seismologic, ...
Filed under: Rock Mechanics -  Rock Falls
Reference: GEOLOGY, November 2014; v. 42; no. 11; p. 1–4; Data Repository item 2014345 | doi:10.1130/G36149.1 | Published online XX Month 2014 © 2014 Geological Society of America
Earthquakes subject tunnel linings to transient strains due to ground shaking, and can cause localized permanent strains in zones of fault rupture. These issues are discussed with respect to seismic analyses and design strategies. Most underground structures ...
Reference: 2012 NZSEE Conference
<p>Since Iran is one of the seismically active regions, and many lessons are embedded in the observations of surface ruptures of Iran earthquakes, the use of case histories as a basis for the development of both insights and engineering judgment is considered. ...
Reference: 6th International Conference on Case Histories in Geotechnical Engineering, Arlington, VA, August 11-16, 2008
The frontal fault system - the Himalayan Frontal Thrust (HFT) associated with the foreland fold - Janauri Anticline, along with other major as well as secondary hinterland thrust faults, provides an ideal site to study the ongoing tectonic activity which has ...
Reference: Journal of Asian Earth Sciences 29 (2007) 604-618
The 2002 M7.9 Denali fault earthquake resulted in 340 km of ruptures along three separate faults, causing widespread liquefaction in the fluvial deposits of the alpine valleys of the Alaska Range and eastern lowlands of the Tanana River. Areas affected by liquefaction ...
Reference: Earthquake Spectra (2004)
A total of 166 observations of sea-level change, 130 measurements of elevation difference, and 16 determinations of horizontal strain provide an excellent view of the (quasi-)static source process of the great 1960 Chilean earthquake.
Reference: Geophys. 1. Int. (1990) 103, 589-598