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Spatio-Temporal Correlation Between Radon Emissions and Seismic Activity: An Example Based on the Vrancea Region (Romania). [PDF]
Montiel-López D +8 more
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A Review of Strain-Distributed Optical Fiber Sensors for Geohazard Monitoring: An Update. [PDF]
Coscetta A +9 more
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Modeling peak ground acceleration for earthquake hazard safety evaluation. [PDF]
Khalid F, Razbin M.
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Reliable earthquake precursors?
Science, 2023Global Positioning System (GPS) measurements suggest hours-long precursors to many large ...
R. Bürgmann
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Earthquake Precursors and Prediction
Encyclopedia of Solid Earth Geophysics, 2011Seiya Uyeda +2 more
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New Opportunities to Study Earthquake Precursors
, 2020New Opportunities to Study Earthquake Precursors Matthew E. Pritchard, Richard M. Allen, Thorsten W. Becker, Mark D. Behn, Emily E. Brodsky, Roland Bürgmann, Cindy Ebinger, Jeff T. Freymueller, Matt Gerstenberger, Bruce Haines, Yoshihiro Kaneko, Steve D.
M. Pritchard +20 more
semanticscholar +1 more source
Episodic aseismic earthquake precursors
Nature, 1988Shallow earthquakes are generally believed to be brittle fractures in a stressed medium with rupture velocity at a speed close to that for shear waves. We know, however, that the Earth allows failure over a wide range of timescales. Creep events occur on the San Andreas fault system, and for some earthquakes the high-speed rupture is accompanied by a ...
Alan T. Linde +4 more
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Earthquake Precursors Based on Rock Acoustic Emission and Deep Learning
The ScientistChina is one of the countries severely affected by earthquakes, making precise and timely identification of earthquake precursors essential for reducing casualties and property damage. A novel method is proposed that combines a rock acoustic emission (AE)
Zihan Jiang +4 more
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Bulletin of the Seismological Society of America, 1975
Abstract An analysis of existing earthquake precursor data leads to a conclusion that the precursors reported so far can be classified into three types, i.e., A1, A2 and B types. Most of type B precursors, observed in terms of anomalous tilts and strains or foreshocks, have no magnitude-dependent precursor time.
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Abstract An analysis of existing earthquake precursor data leads to a conclusion that the precursors reported so far can be classified into three types, i.e., A1, A2 and B types. Most of type B precursors, observed in terms of anomalous tilts and strains or foreshocks, have no magnitude-dependent precursor time.
openaire +1 more source

