[PDF] Top 20 Source mechanism of the 23 October, 2011, Van (Turkey) earthquake (Mw = 7 1) and aftershocks with its tectonic implications
Has 10000 "Source mechanism of the 23 October, 2011, Van (Turkey) earthquake (Mw = 7 1) and aftershocks with its tectonic implications" found on our website. Below are the top 20 most common "Source mechanism of the 23 October, 2011, Van (Turkey) earthquake (Mw = 7 1) and aftershocks with its tectonic implications".
Source mechanism of the 23 October, 2011, Van (Turkey) earthquake (Mw = 7 1) and aftershocks with its tectonic implications
... Lake Van Basin have the poten- tial to produce earthquakes with magnitude greater than ...of Van city center ( ¨ Orc¸en et ...an earthquake of mag- nitude greater than six (M > 6) (Wells and ... See full document
13
Coulomb static stress changes before and after the 23 October 2011 Van, eastern Turkey, earthquake ( W7.1): implications for the earthquake hazard mitigation
... the aftershocks, the northeastern aftershock cluster in ...of 2011 Van earthquake indicate that the mainshock rupture bolstered stress over both the east- ern ...ing aftershocks in the ... See full document
14
Engineering geologic assessment of the slope movements and liquefaction failures of the 23 October 2011 Van earthquake
... of Turkey, on 23 October 2011. The earthquake was felt over a large area in the East Anatolia ...the earthquake epicenters that are reported by different seismological networks, ... See full document
14
Initial 30 seconds of the 2011 off the Pacific coast of Tohoku Earthquake (Mw 9 0)—amplitude and τc for magnitude estimation for Earthquake Early Warning—
... many earthquake events and many recording stations, with differences in the distance between source and recording stations: many of them were from less than 100 km, and some were from larger than 100 km for ... See full document
5
Large intraslab earthquake (2011 April 7, M 7 1) after the 2011 off the Pacific coast of Tohoku Earthquake (M 9 0): Coseismic fault model based on the dense GPS network data
... Miyagi-oki earthquake (Miura et ...at 1-second or 2-second intervals through dual-frequency receivers at all ...the 2011, M 9, earthquake that the GPS data from these sites are defi- nitely ... See full document
5
Relation between similar aftershocks and ruptured asperity of a large inland earthquake: Example of the 2007 Noto Hanto earthquake
... the source radius estimated by the circular crack model (Brune, 1970) with a constant stress ...the source fault (dotted rectangle with the solid line as the upper edge) (Horikawa, 2008) and the station ... See full document
5
Spatial distribution and focal mechanisms of aftershocks of the 2011 off the Pacific coast of Tohoku Earthquake
... the aftershocks exhibited a variety of focal ...Interplate aftershocks with thrust focal mechanisms did not occur within the large coseismic slip area estimated from GPS data but instead occurred in the ... See full document
5
Damages to unreinforced masonry buildings by the Van earthquakes of 23 October and 9 November 2011
... In a seismic-resistant masonry building, crossing walls have to be interlocked properly to improve out-of-plane strength. The problem of unconnected intersecting walls is very com- mon in the region (Fig. 9). Due to bad ... See full document
9
Characteristics of relocated hypocenters of the 2018 M6 7 Hokkaido Eastern Iburi earthquake and its aftershocks with a three dimensional seismic velocity structure
... Iburi earthquake and its surrounding area, using a three-dimensional seismic structure, the double-difference relocation method, and the JMA earthquake ...and its aftershocks are ... See full document
11
Rise time and source duration of the 2008 MW 7 9 Wenchuan (China) earthquake as revealed by Rayleigh waves
... entire source duration is ∼ ...during earthquake fault- ing, ...the source area within the crust ranges from ...Chi-Chi earthquake and the 2004 great Sumatra earth- quake ...(China) ... See full document
8
Preceding seismic activity and slow slip events in the source area of the 2011 Mw 9.0 Tohoku-Oki earthquake: a review
... Tohoku-Oki earthquake, there occurred a long-term transient ...the source area on the megathrust ...approximately 1 day before the Tohoku-Oki earthquake, no significant accel- erating preslip ... See full document
13
Seismogenic fault and tectonic significance of 1996 Karakoram Pass earthquake (Ms 7 1) based on InSAR
... Fig. 1 Location and regional tectonic background of the 1996 Karakoram Pass ...the earthquake epicenter, the red lines are traces of faults from Central Asia Fault Database, and the purple arrows ... See full document
11
Slip on a mapped normal fault for the 28th December 1908 Messina earthquake (Mw 7 1) in Italy
... Messina earthquake (Mw ...transformed earthquake science by triggering the study of earthquake environmental effects worldwide, yet its source is still a matter of ...the ... See full document
9
Source model of the 2007 Noto Hanto earthquake (Mw 6 7) for estimating broad band strong ground motion
... the source area of the mainshock is divided into N × N meshes, and the mesh size (x) × (w) is determined by the source area of the aftershock whose records are used as the empirical Green’s ...the ... See full document
6
Normal faulting stress state associated with low differential stress in an overriding plate in northeast Japan prior to the 2011 Mw 9 0 Tohoku earthquake
... the 2011 Tohoku earthquake and co- and post-seismic deformation of the M7 class earthquakes around Iwaki ...January 1, 2002, to March 1, ...al. 2011) are also marked: (A) August 16, ... See full document
8
Outline of the 2011 off the Pacific coast of Tohoku Earthquake (Mw 9 0) —Earthquake Early Warning and observed seismic intensity—
... issued Earthquake Early Warning (EEW) announcements to the general public of the Tohoku district and then the warning was automatically broadcast through TV, radios and cellular phone ...intensity 7 was ... See full document
5
Coulomb stresses imparted by the 25 March 2007 Mw=6 6 Noto Hanto, Japan, earthquake explain its ‘butterfly’ distribution of aftershocks and suggest a heightened seismic hazard
... an earthquake have been used to explain the spatial distri- bution of the subsequent aftershocks (Stein, 1999; Steacy et ...large earthquake trig- gering ... See full document
6
Strong aftershocks in the northern segment of the Wenchuan earthquake rupture zone and their seismotectonic implications
... and its extension towards the northeast, the Chaba-LinAnsiAn fault ...most aftershocks close to the faulting plane show mechanisms similar to that of the main shock, accu- rate mechanisms of ... See full document
6
Van earthquakes (23 October 2011 and 9 November 2011) and performance of masonry and adobe structures
... surrounding Van Lake, different rock units and alluvial deposits formed between Paleozoic and Holocene are ...observed. Van Lake region includes metamorphic rocks belonging to the Bitlis massive to the ... See full document
6
DInSAR Coseismic Deformation of the May 2011 M w5.1 Lorca Earthquake (southeastern Spain)
... Using the numerical model as reference for the coseismic displacement, we found a good agreement between the DIn- SAR measurements (3 cm) and the model estimated values (4 cm) on the northern hanging wall block of the ... See full document
9
Related subjects