scholarly journals Three-Dimensional Tomography of Ionospheric Anomalies Immediately Before the 2015 Illapel Earthquake, Central Chile

2018 ◽  
Vol 123 (5) ◽  
pp. 4015-4025 ◽  
Author(s):  
Liming He ◽  
Kosuke Heki
Keyword(s):  
Three Dimensional ◽  
Central Chile ◽  
2015 Illapel Earthquake ◽  
Illapel Earthquake

scholarly journals The 2015 Illapel earthquake, central Chile: A type case for a characteristic earthquake?

2016 ◽  
Vol 43 (2) ◽  
pp. 574-583 ◽  
Author(s):  
F. Tilmann ◽  
Y. Zhang ◽  
M. Moreno ◽  
J. Saul ◽  
F. Eckelmann ◽  
...  
Keyword(s):  
Characteristic Earthquake ◽  
Central Chile ◽  
2015 Illapel Earthquake ◽  
Illapel Earthquake

The 16 September 2015 Illapel Earthquake and Tsunami: Post-Event Tsunami Inundation, Building and Infrastructure Damage Survey in Coquimbo, Chile

2021 ◽  
Author(s):  
Ryan Paulik ◽  
James H. Williams ◽  
Nick Horspool ◽  
Patricio A. Catalan ◽  
Richard Mowll ◽  
...  
Keyword(s):  
Tsunami Inundation ◽  
Damage Survey ◽  
2015 Illapel Earthquake ◽  
Illapel Earthquake

Far-field tsunami data assimilation for the 2015 Illapel earthquake

2019 ◽  
Vol 219 (1) ◽  
pp. 514-521 ◽  
Author(s):  
Y Wang ◽  
K Satake ◽  
R Cienfuegos ◽  
M Quiroz ◽  
P Navarrete
Keyword(s):  
Data Assimilation ◽  
Near Field ◽  
Source Parameters ◽  
Deep Ocean ◽  
Seismic Source ◽  
Far Field ◽  
Complementary Method ◽  
East Pacific ◽  
2015 Illapel Earthquake ◽  
Illapel Earthquake

SUMMARY The 2015 Illapel earthquake (Mw 8.3) occurred off central Chile on September 16, and generated a tsunami that propagated across the Pacific Ocean. The tsunami was recorded on tide gauges and Deep-ocean Assessment and Reporting of Tsunami (DART) tsunameters in east Pacific. Near-field and far-field tsunami forecasts were issued based on the estimation of seismic source parameters. In this study, we retroactively evaluate the potentiality of forecasting this tsunami in the far field based solely on tsunami data assimilation from DART tsunameters. Since there are limited number of DART buoys, virtual stations are assumed by interpolation to construct a more complete tsunami wavefront for data assimilation. The comparison between forecasted and observed tsunami waveforms suggests that our method accurately forecasts the tsunami amplitudes and arrival time in the east Pacific. This approach could be a complementary method of current tsunami warning systems based on seismic observations.

SOAR Telescope seismic performance I: impact of the 2015 Illapel earthquake

2016 ◽  
Author(s):  
Jonathan H. Elias ◽  
Michael Warner ◽  
Freddy Muñoz ◽  
Gerardo Gómez
Keyword(s):  
Seismic Performance ◽  
2015 Illapel Earthquake ◽  
Illapel Earthquake

The delayed aftershocks of the Illapel Earthquake Mw 8.3, 2015, Chile

2021 ◽  
Author(s):  
Franco Lema ◽  
Mahesh Shrivastava
Keyword(s):  
Tide Gauge ◽  
Stress Transfer ◽  
Large Earthquake ◽  
Seismic Source ◽  
Coulomb Stress ◽  
Coulomb Stress Changes ◽  
Finite Fault ◽  
Stress Changes ◽  
2015 Illapel Earthquake ◽  
Illapel Earthquake

<p>The delayed aftershocks 2018 Mw 6.2 on April 10 and Mw 5.8 on Sept 1 and 2019 Mw 6.7 on January 20, Mw 6.4 on June 14, and Mw 6.2 on November 4, associated with the Mw 8.3 2015 Illapel Earthquake occurred in the ​​central Chile. The seismic source of this earthquake has been studied with the GPS, InSAR and tide gauge network. Although there are several studies performed to characterize the robust aftershocks and the variations in the field of deformation induced by the megathrust, but there are still aspects to be elucidated of the relationship between the transfer of stresses from the interface between plates towards delayed aftershocks with the crustal structures with seismogenic potential. Therefore, the principal objective of this study is to understand how the stress transfer induced by the 2015 Illapel earthquake of the heterogeneous rupture mechanism to intermediate-deep or crustal earthquakes. For this, coulomb stress changes from  finite fault model of the Illapel earthquake and with the biggest aftershocks in year 2015 are used. These cumulative stress pattern provides substantial evidences for the delayed aftershocks in this region. The subducting Challenger Fault Zone and Juan Fernandez Ridge heterogeneity are existing feature, which releases the accumulated coulomb stress changes and provide delayed aftershocks.  Therefore along with stress induced by a large earthquake such as Mw 8.3 from Illapel 2015 along with biggest aftershocks, have a direct mechanism that may activate the  delayed aftershocks. Our study suggests  the activation of crustal faults in this research as a risk assessment factor for the evaluating in the seismic context of the region and useful for another subduction zone.</p>

scholarly journals Aftershock seismicity and tectonic setting of the 2015 September 16 Mw 8.3 Illapel earthquake, Central Chile

2016 ◽  
Vol 206 (2) ◽  
pp. 1424-1430 ◽  
Author(s):  
Dietrich Lange ◽  
Jacob Geersen ◽  
Sergio Barrientos ◽  
Marcos Moreno ◽  
Ingo Grevemeyer ◽  
...  
Keyword(s):  
Subduction Zone ◽  
Tectonic Setting ◽  
Continental Margins ◽  
Detailed Knowledge ◽  
Coseismic Slip ◽  
Central Chile ◽  
Rupture Area ◽  
Significant Damage ◽  
Illapel Earthquake ◽  
Subduction Zone Earthquakes

Abstract Powerful subduction zone earthquakes rupture thousands of square kilometres along continental margins but at certain locations earthquake rupture terminates. To date, detailed knowledge of the parameters that govern seismic rupture and aftershocks is still incomplete. On 2015 September 16, the Mw 8.3 Illapel earthquake ruptured a 200 km long stretch of the Central Chilean subduction zone, triggering a tsunami and causing significant damage. Here, we analyse the temporal and spatial pattern of the coseismic rupture and aftershocks in relation to the tectonic setting in the earthquake area. Aftershocks cluster around the area of maximum coseismic slip, in particular in lateral and downdip direction. During the first 24 hr after the main shock, aftershocks migrated in both lateral directions with velocities of approximately 2.5 and 5 km hr−1. At the southern rupture boundary, aftershocks cluster around individual subducted seamounts that are related to the downthrusting Juan Fernández Ridge. In the northern part of the rupture area, aftershocks separate into an upper cluster (above 25 km depth) and a lower cluster (below 35 km depth). This dual seismic–aseismic transition in downdip direction is also observed in the interseismic period suggesting that it may represent a persistent feature for the Central Chilean subduction zone.

Three-dimensional local earthquake tomography of pre-Cenozoic structures in the coastal margin of central Chile: Pichilemu fault system

2021 ◽  
Vol 25 (2) ◽  
pp. 521-533
Author(s):  
Daniela Calle-Gardella ◽  
Diana Comte ◽  
Marcelo Farías ◽  
Steven Roecker ◽  
Andreas Rietbrock
Keyword(s):  
Three Dimensional ◽  
Fault System ◽  
Central Chile ◽  
Local Earthquake Tomography ◽  
Coastal Margin ◽  
Local Earthquake

scholarly journals Coseismic Fault Model of Mw 8.3 2015 Illapel Earthquake (Chile) Retrieved from Multi-Orbit Sentinel1-A DInSAR Measurements

2016 ◽  
Vol 8 (4) ◽  
pp. 323 ◽  
Author(s):  
Giuseppe Solaro ◽  
Vincenzo De Novellis ◽  
Raffaele Castaldo ◽  
Claudio De Luca ◽  
Riccardo Lanari ◽  
...  
Keyword(s):  
Fault Model ◽  
2015 Illapel Earthquake ◽  
Illapel Earthquake
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