نتایج جستجو برای: mainshock

تعداد نتایج: 432  

2014
M M Moro M. C V Cannelli V. C M Chini M. B C Bignami C. M D Melini D. S S Stramondo S. S M Saroli M. P M Picchiani M. K C Kyriakopoulos C. B C A Brunori C. A.

The present work reports the analysis of a possible relationship due to stress transfer between the two earthquakes that hit the province of Van, Eastern Turkey, on October 23, 2011 (Mw = 7.2) and on November 9, 2011 (Mw = 5.6). The surface displacement field of the mainshock has been obtained through a combined data set made up of differential interferograms from COSMO-SkyMed and ENVISAT satel...

2013
Kazumasa Oguri Kiichiro Kawamura Arito Sakaguchi Takashi Toyofuku Takafumi Kasaya Masafumi Murayama Katsunori Fujikura Ronnie N. Glud Hiroshi Kitazato

In situ video observations and sediment core samplings were performed at two hadal sites in the Japan Trench on July, 2011, four months after the Tohoku-Oki earthquake. Video recordings documented dense nepheloid layers extending ~30-50 m above the sea bed. At the trench axis, benthic macrofauna was absent and dead organisms along with turbid downslope current were observed. The top 31 cm of se...

2002
Gert Zöller Sebastian Hainzl

[1] The critical point hypothesis for large earthquakes predicts two different precursory phenomena in space and time, an accelerating moment release and the growth of the spatial correlation length. The objective of this work is to investigate both methods with respect to their predictive power. A systematic statistical test based on appropriate random earthquake catalogs allows to quantify th...

1998
David P. Schaff Gregory C. Beroza Bruce E. Shaw

The recurrence intervals of repeating earthquakes on the San Andreas Fault in the Loma Prieta aftershock zone follow the characteristic 1/t decay of Omori’s law. A model in which these earthquakes occur on isolated patches of the fault that fail in stick-slip with creep around them can explain this observation. In this model the recurrence interval is inversely proportional to the loading rate ...

2000
Y. Y. Kagan

Statistical verification of the VAN or SES (seismic electric signals) predictions from 1987-1989 is considered. The test is carried out with the updated ruies proposed by Varotsos et al. [1996]. Although for the Greek (SI-NOA) earthquake catalog the VAN method formally is successful, this high rate of success is due either to the retroactive adjustment of prediction rules or to the non-randomne...

2016
Aitaro Kato Jun’ichi Fukuda Takao Kumazawa Shigeki Nakagawa

The earthquake nucleation process has been vigorously investigated based on geophysical observations, laboratory experiments, and theoretical studies; however, a general consensus has yet to be achieved. Here, we studied nucleation process for the 2014 Iquique, Chile Mw 8.2 megathrust earthquake located within the current North Chile seismic gap, by analyzing a long-term earthquake catalog cons...

2012
Xiaofeng Meng Xiao Yu Zhigang Peng Bo Hong

The recently developed matched filter technique is effective in detecting earthquakes during intensive aftershock or swarm sequences. However, currently our detection code can only process on single-CPU computers, which takes a long time to perform the cross-correlation between continuous seismic data and template events. In this paper, we present a GPU-based computation method to significantly...

Journal: :Frontiers in Earth Science 2022

In the period between December 2018 and July 2019, a series of earthquakes (EQs), including 16 Ms 5.7 Xingwen mainshock 17 June 2019 6.0 Changning mainshock, struck shale gas exploration field in southern margin Sichuan Basin. The EQs both occurred on concealed faults, which led to hundreds casualties, affected total over 160 thousand people Sichuan. aftershock sequences following were clustere...

2007
Emily E. Brodsky Vassilis Karakostas Hiroo Kanamori

The M•,=7.4 Izmit, Turkey earthquake triggered widespread regional seismicity in Greece over a study region extending from 400 km to nearly 1000 km away from the epicenter. Small events began immediately after the passage of the mainshock surface waves suggesting that the transient stresses of the seismic waves were the trigger. The increase in cataloged earthquakes in ordinary continental crus...

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