نتایج جستجو برای: earthquake magnitude

تعداد نتایج: 167554  

Journal: :Science 1993
D P Hill P A Reasenberg A Michael W J Arabaz G Beroza D Brumbaugh J N Brune R Castro S Davis D Depolo W L Ellsworth J Gomberg S Harmsen L House S M Jackson M J Johnston L Jones R Keller S Malone L Munguia S Nava J C Pechmann A Sanford R W Simpson R B Smith M Stark M Stickney A Vidal S Walter V Wong J Zollweg

The magnitude 7.3 Landers earthquake of 28 June 1992 triggered a remarkably sudden and widespread increase in earthquake activity across much of the western United States. The triggered earthquakes, which occurred at distances up to 1250 kilometers (17 source dimensions) from the Landers mainshock, were confined to areas of persistent seismicity and strike-slip to normal faulting. Many of the t...

2000
Dominique Derauw

The 17 of August 1999, an important earthquake of magnitude 7.6 occurred along the North Anatolian fault in the area of Izmit (Turkey). Relative horizontal displacements up to 4.5 meters were observed. The epicenter of the earthquake under concern is located in Golcuk, near the city of Izmit, on the South border of the Marmara Sea. The fault in the vicinity of Izmit is mainly oriented along an ...

Journal: :Science 2005
Robert M Nadeau David Dolenc

We have discovered nonvolcanic tremor activity (i.e., long-duration seismic signals with no clear P or S waves) within a transform plate boundary zone along the San Andreas Fault near Cholame, California, the inferred epicentral region of the 1857 Fort Tejon earthquake (moment magnitude approximately 7.8). The tremors occur between 20 to 40 kilometers' depth, below the seismogenic zone (the upp...

Journal: :geopersia 0
nasser naimi-ghassabian department of geology, faculty of earth sciences, university of birjand, birjand, iran mohammad-mahdi khatib department of geology, faculty of earth sciences, university of birjand, birjand, iran hamid nazari research institute for earth sciences, geological survey of iran , mahmoud-reza heyhat department of geology, faculty of earth sciences, university of birjand, birjand, iran

the gutenberg–richter parameters (a and b), fractal dimension (dc), and relationships between these parameters are calculated for different regions of the north of central-east iran blocks (nceib). the whole examined area (between 34°-36° n and 55°-61° e) is divided into 55 equal square grids. both the a and b values for the frequency-magnitude distribution (fmd) and the fractal dimension (dc) ...

2007
Abhijit Ghosh Andrew V. Newman Zhigang Peng

ACKNOWLEDGEMENTS I would like to thank my primary advisor Dr. Andrew V. Newman for providing his excellent guidance and scientific insight throughout the study. I am thankful to Dr. for their thoughtful advice and suggestions. I am grateful to Dr. Tapas Bhattacharyya for the stimulating discussions and his support. I would also like to thank numerous prior and recent earthquake analysts, includ...

2008

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Journal: :فیزیک زمین و فضا 0
حمیدرضا جوان امروز گروه فیزیک زمین، مؤسسه ژئوفیزیک دانشگاه تهران مرتضی اسکندری قادی دانشکده مهندسی عمران، پردیس دانشکده های فنی دانشگاه تهران نوربخش میرزائی گروه فیزیک زمین، مؤسسه ژئوفیزیک دانشگاه تهران

ground vibrations during an earthquake can severely damage structures and equipments housed in them. many factors including earthquake magnitude, distance from the fault or epicenter, duration of strong shaking, soil condition of the site, and the frequency content of the motion define the properties of ground motion and its amplification. a deep understanding of the effects of these factors on...

ژورنال: کواترنری ایران 2018
Zare, Mehdi,

On November 12, 2017, at 18:18 UTC, a major earthquake with moment magnitude Mw7.3 struck the Kermanshah province of Iran, causing extended damage and casualties. Thus, we explore seismicity preceding this earthquake, with the aim to understand whether the information from past events could provide some insights about the occurrence of this and other future large earthquakes. Taking into accou...

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