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Oceanic intraplate earthquakes: Implications for local and regional intraplate stress

Journal of Geophysical Research: Solid Earth, 1980
Focal mechanisms of intraplate earthquakes provide the only means at present by which to characterize the long‐wavelength tectonic stress field in oceanic lithosphere. Stress orientations inferred from focal mechanisms may not accurately reflect the state of stress in the epicentral area, however, or the measured stresses may be dominated by local ...
Eric A. Bergman, Sean C. Solomon
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DISPLACEMENT MODELLING OF INTRAPLATE EARTHQUAKES

ISET Journal of Earthquake Technology, 2004
This paper presents the case for a displacement-based approach for the seismic design and performance assessment of structures in intraplate regions. A newly established model for predicting seismic displacement demand is introduced. The presented material is based on outcomes from research which integrates expertise in the fields of engineering ...
Lam, Nelson T., Wilson, John L.
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Intraplate earthquakes in the Svalbard Archipelago

Journal of Geophysical Research: Solid Earth, 1979
A small, seismically active region, designated the Heerland seismic zone, has been delineated in the Svalbard archipelago. Over 500 earthquakes in this region, of which nearly 50 were reliably located, were recorded during a 9‐week field season in 1977.
Brian J. Mitchell   +4 more
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A Nonlinear Model for Intraplate Earthquake

2020
Intraplate earthquakes are very hazardous disaster for human’s society. The features of earthquake-generating process are discussed in this paper by using a dynamic nonlinear model with Chinese Continental area as an example. The theoretical computation result of the model shows similarity to the real seismicity in Mainland China.
Li Li, Zhang Guomin, Shi Yaolin
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Intraplate Earthquakes

2014
Intraplate earthquakes occur away from tectonic plate boundaries: their locations are difficult to predict, risking huge damage and loss of life. The 2001 Bhuj earthquake (featured in this book) was the largest intraplate earthquake for three decades and has provided unique insight into these events. This cutting-edge book brings together research from
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Intraplate Earthquakes in Iceland

1989
Only a small proportion of Icelandic earthquakes is not directly associated with the mid-Atlantic plate boundary that crosses the island. These intraplate earthquakes fall mainly into two classes. In the first class are earthquakes occurring west of the main rift zone through Iceland, within the tongue of lithosphere that is bounded by the two ...
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Three-level Tectonic Model for Intraplate Earthquakes

Earth Science Frontiers, 2009
Abstract Earthquake is a process concerning the long-term accumulation and abrupt release of energy in nature. On the basis of the analysis of the characteristics of intraplate earthquake, we present a three-level tectonic model for intraplate earthquake.
Yang Weiran   +5 more
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BUILDING DUCTILITY DEMAND: INTERPLATE VERSUS INTRAPLATE EARTHQUAKES

Earthquake Engineering & Structural Dynamics, 1996
The inelastic seismic response behaviour for a range of simplified single-degree-of-freedom models has been analysed using 180 random phase angle synthetic accelerograms with different frequency contents and different durations and 105 real accelerograms collected from different regions worldwide.
N. LAM, J. WILSON, G. HUTCHINSON
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Attenuation models inferred from intraplate earthquake recordings

Earthquake Engineering & Structural Dynamics, 1990
AbstractStrong‐motion recordings at 87 sites from 56 different intraplate earthquakes from North America, Europe, China and Australia have been used through a two‐step regression analysis to develop new attenuation models for peak ground acceleration, and for pseudo‐relative velocity for frequencies of 0.25, 0.5, 1.0, 2.0, 5.0 and 10.0 Hz, all for 5 ...
Anders Dahle   +2 more
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On the nature of intraplate earthquakes

Journal of Seismology, 2016
Continental intraplate regions are characterized by uniform stresses over thousands of kilometers. Local stresses, with wavelengths of tens to hundreds of kilometers can accumulate at inhomogeneities lying within these regional fields. A variety of geological structures, herein called local stress concentrators (LSCs), act as elastic inhomogeneities ...
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