Results 101 to 110 of about 7,837 (204)
Investigation of the time and magnitude distribution<br />of the fore- and aftershocks of the Cremasta lake earthquake which occurred<br />on February 5, 1966 is made.
B. PAPAZACHOS +3 more
doaj +1 more source
. The monitoring of statistical network properties could be useful for the short-term hazard assessment of the occurrence of mainshocks in the presence of foreshocks. Using successive connections between events acquired from the earthquake catalog of the
E. Daskalaki +4 more
semanticscholar +1 more source
Seismic Hazard Assessment For Peninsular Malaysia Using Gumbel Distribution Method [PDF]
This Paper Presents The Preliminary Study On Seismic Hazard Assessment Which Involved Developing Macrozonation Map For Two Hazard Levels, I.E. 10% And 2% Probabilities Of Exceedance In 50 Years For Bedrock Of Peninsular Malaysia.
Adnan, Azlan +3 more
core
On certain aftershock and foreshock parameters in the area of Greece
Published information (l2) on the aftershocks and foreshocks of many principal shallow earthquakes occurred in the area of Greece between 1911 and 1973 constitutes a more or less homogeneous and complete sample of data in respect to some ...
B. C. PAPAZACHOS
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Wei-Jin Dynasty: Talking about seismic activity
Talking about China’s seismicity research inevitably involves an outstanding female scientist, Mei Shirong. She does not have the title of academician, but is recognized and irreplaceable as an academic leader in the field of earthquake prediction in ...
Rui Feng
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In this paper, the investigation of the dynamic response of a cable-stayed footbridge with steel reinforced concrete deck to foreshocks, a mainshock and an aftershock seismic sequence is delivered.
Ciura Rafał +2 more
doaj +1 more source
Months-long seismicity transients preceding the 2023 MW 7.8 Kahramanmaraş earthquake, Türkiye. [PDF]
Kwiatek G +8 more
europepmc +1 more source
Editorial: Pre-, co-, and post-seismic processes of recent earthquakes in mainland China
Huaizhong Yu +2 more
doaj +1 more source
Foreshocks are the most obvious signature of the earthquake nucleation stage and could, in principle, forewarn of an impending earthquake. However, foreshocks are only sometimes observed, and we have a limited understanding of the physics that controls ...
David C. Bolton +5 more
doaj +1 more source
This study analyzed and summarized in detail the spatial and temporal distributions of earthquakes, tidal responses, focal mechanisms, and stress field characteristics for the M 7.3 Haicheng earthquake sequence in February 1975.
Xinglin Lei +3 more
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