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Magnitude Scaling Relationships - GEM Nexus
Magnitude Scaling Relationships - GEM Nexus

... provide general guidance for regression selection in seismic hazard modelling. Our compilation is limited to regressions of magnitude (or seismic moment) on source area or length. It is a representative but not exhaustive compilation of the available regressions around the world. ...
Deliverable 3.2 - version 2 - Website for the dissemination of long
Deliverable 3.2 - version 2 - Website for the dissemination of long

... complemented with the descriptions of the steps that the SHARE catalogue underwent since its first release in April 2011, which are briefly summarized in the following. 1. SHEEC was first released on 13 April 2011, as deliverable D3.2 of the Project. The catalogue was made available as two separate ...
Relocating a Cluster of Earthquakes Using a Single
Relocating a Cluster of Earthquakes Using a Single

Short-Term Earthquake Hazard Assessment for
Short-Term Earthquake Hazard Assessment for

Earthquake Energy Release Mechanism Ahmed Elgamal
Earthquake Energy Release Mechanism Ahmed Elgamal

Moment Magnitude Estimates for Earthquakes in the Greek Region
Moment Magnitude Estimates for Earthquakes in the Greek Region

Possible stress states adjacent to the rupture
Possible stress states adjacent to the rupture

Anomalous stress diffusion in earthquake triggering: Correlation
Anomalous stress diffusion in earthquake triggering: Correlation

Observations and Tectonic Setting of Historic
Observations and Tectonic Setting of Historic

A BENEFIT/COST ANALYSIS FOR THE SEISMIC REHABILITATION
A BENEFIT/COST ANALYSIS FOR THE SEISMIC REHABILITATION

... father Zeki who have been particularly supportive and patient, for believing in me. The number of people that have contributed to both my personal and educational life during the last three years is too many to list them explicitly, so rather than risking forgetting anybody, I would just like to tha ...
2002/005 OFFSHORE TECHNOLOGY REPORT Seismic hazard: UK continental shelf
2002/005 OFFSHORE TECHNOLOGY REPORT Seismic hazard: UK continental shelf

... area to steadily subside, with only minor faults involved. By the end of the Alpine Orogeny, all basinal areas subsided. Subsidence was not uniform, yet its main axis followed the N-S graben trends. The regional downwarping of the North Sea area lasted into Quaternary times, although with varying ra ...
Seismic vulnerability of the Himalayan half-dressed rubble
Seismic vulnerability of the Himalayan half-dressed rubble

... offices, health care units, etc. The aim of the experimental study was to understand the damage mechanism of the model, develop damage scale towards deformation-based assessment and retrieve the lateral force-deformation response of the model besides its elastic dynamic properties, i.e. fundamental ...
Segmentation of seismicity along the Himalayan Arc due to
Segmentation of seismicity along the Himalayan Arc due to

Preliminary results of a paleoseismological analysis along the Sahel
Preliminary results of a paleoseismological analysis along the Sahel

Earthquake scaling relations for mid
Earthquake scaling relations for mid

Seismicity models based on Coulomb stress calculations
Seismicity models based on Coulomb stress calculations

SLOPE FAILURES AND PALEOSEISMICITY, EFFINGHAM INLET,
SLOPE FAILURES AND PALEOSEISMICITY, EFFINGHAM INLET,

... 1. Introduction In southwestern British Columbia and the U.S. Pacific Northwest, a region collectively known as “Cascadia”, the instrumental record of earthquake activity is short (less than 130 years). Southwestern British Columbia alone experiences more than 200 crustal and intraplate earthquakes ...
Intricacies of the Himalayan seismotectonics and seismogenesis
Intricacies of the Himalayan seismotectonics and seismogenesis

Tsunami - Tulane University
Tsunami - Tulane University

... the earthquake, had a run-up 30 m and completely destroyed the lighthouse. 4.5 hours later the same tsunami reached the Hawaiian Islands after traveling at an average speed of 659 km/hr. As it approached the city of Hilo on the Big Island, it slowed to about 47 km/hr (note that even the fastest huma ...
A probabilistic seismic hazard assessment of the Trans
A probabilistic seismic hazard assessment of the Trans

... B) fits separately the instrumental and the historical data and merge the two fits into one curve. A uniform seismic hazard (USH) of the TMVB for a return period of 500 years was calculated considering three major sources of earthquakes: 1) Subduction thrust-faulting events in the Middle American Tr ...
Historical tsunami in the Makran Subduction Zone off
Historical tsunami in the Makran Subduction Zone off

Long-Term Records of Tsunamis
Long-Term Records of Tsunamis

Earthquake Disaster Guidelines - National Disaster Management
Earthquake Disaster Guidelines - National Disaster Management

... and technical institutions, academics, technocrats, architects and humanitarian organizations. The first such meeting was held on 21 December 05. It reviewed the status of earthquake management efforts thus far, identified gaps and set the framework for the approach. Thereafter, a Core Group was con ...
Entire paper as a 2 MB  file
Entire paper as a 2 MB file

102_2012_Wang_et_al_.. - Description
102_2012_Wang_et_al_.. - Description

... in Taipei and Taichung are found comparable, and both are higher than those of Kaohsiung. The higher rate in Taipei and Taichung results from their location being closer to the subduction zone located in the eastern offshore, where a high concentration of earthquakes is observed in Fig. 1. In contra ...
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2010 Pichilemu earthquake



The 2010 Pichilemu earthquake (Spanish: Terremoto de Pichilemu de 2010), also known as the Libertador O'Higgins earthquake, was a 6.9 MW intraplate earthquake that struck Chile's O'Higgins Region on 11 March 2010. The earthquake was centred 15 kilometres (9.3 mi) northwest of the city of Pichilemu, according to the University of Chile Seismological Service.The earthquake was caused by increased regional stress arising from an earthquake on 27 February, centered offshore Maule Region, which was felt throughout central Chile. The 11 March earthquake was at first thought to be an aftershock from the 27 February event, but University of Chile Seismologist Jaime Campos identified it as an ""independent earthquake"". The Hawaii-based Pacific Tsunami Warning Center pointed out the possibility of local tsunamis within 100 kilometres (62 mi) of the epicentre, although small, but violent waves were seen in the Pichilemu and Bucalemu area. One person was reported dead. At least eleven aftershocks immediately followed, causing panic throughout coastal towns between the Coquimbo and Los Lagos regions.The earthquake was specially destructive in the epicentre town, Pichilemu, capital of Cardenal Caro Province. The city hosts five National Monuments of Chile, of which two, the Agustín Ross Park and the Agustín Ross Cultural Centre, were seriously damaged by the earthquake. It also damaged the villages of La Aguada and Cardonal de Panilonco. Rancagua, the capital of O'Higgins Region, was also damaged, leading President Sebastián Piñera to declare a catastrophe state in O'Higgins Region.
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