Modelos de fuente sismica finita. Modelo de falla circular. Modele de Haskell
|
|
- Roy Greer
- 6 years ago
- Views:
Transcription
1 Modelos de fuente sismica finita Modelo de falla circular Modele de Haskell
2 Nacimiento de la dinamica de la fuente A principios de los años 1970 : Aki (1967) Scaling law of earthquake spectra Kostrov (1964, 1966) Circular crack, 2D crack, Energy Brune (1970) Circular crack body wave spectrum Madariaga (1976) put together all this. R 2 Parametros: Mo R No definen la velocidad de ruptura
3 Ley de escalamiento de Aki Size Hay una sola escala de longitud: Radio R o L Mo σ R 3
4 Ley de escala de los terremotos Magnitude (M w ) Moment (Nm) Longueur (km) Durée (s) Glissement (m) ? 300? 100?
5 n Slip of a circular crack stress D 24 Δσ 7π μ 2 2 ( ) R r r = Average slip R D = 16 Δσ 7π μ R
6 Deslizamiento u Modelo de ruptura sismica circular (3D) 2R L (x o -x) 1/2 Distribution de deslizamiento eliptica Esfuerz o 1/(x-x o ) 1/2 Concentration de esfuerzos Augmentation de contrainte x x o L chute de contrainte constant Caida de esfuerzo D 24 Δσ 7π μ 2 2 ( r) = R r
7 Modelo de fisura circular estática Deslizamiento D r) 24 Δσ 7π μ 2 2 ( R r = Deslizamiento medio D = 16 Δσ 7π μ R Momento sísmico 3 M 0 = 16 Δσ 7 R Energia de deformacion W = 8 7 Δσ μ 2 R 3
8 Fundamentals of earthquake scaling Surface Μ 0 = σ R 3 Signal R R σ R 2 R 0 Mo R 2 0 t R 2 Spectrum R 3 R -1 f R 0 3 R 0-1
9 Fundamentals of earthquake scaling Surface R Displacement Signal R 2 Velocity Signal R t R R 2 Acceleration Signal 1 Spectrum R 3 R -1 f
10 Modelo de escalamiento de la fuente Deslizamiento medio D = 16 Δσ 7π μ R Momento sísmico M 0 = 16 7 Δσ R 3 Frecuencia esquina f c = 0.37 β R Momento vs. frecuencia M 0 3 fc
11 Escalamiento de momento y corner frequency Momento sismico Mw Corner frequency f c M 0 3 fc Frecuencia f
12 Modern test of earthquake scaling law Prieto, Shearer and Vernon, JGR, 2004
13 Spectral analysis of California earthquakes P wave S wave
14 Modern tests of earthquake scaling law individual collapsed Test by Prieto et al JGR, 2004 f p / =1.6 f p f s Circular crack model / =1.7 f p f s f s ( Madariaga, 76)
15 The Tocopilla Earthquake of 21 November 2007 A double event at the bottom of the plate interface Mw=7,8 Mo = 2, Nm From Peyrat et al (GJI 2010) Inverted triangles accelerograms In red PBO stations used for this study
16 The Tocopilla earthquake sequence in Northern Chile Main event Mw 7.7 on 14 November 2007 Two main aftershocks on 15 November 2007 Deep slab push aftershock 16 December 2007
17 Spectral stack of a set Tocopilla aftershocks Q From Lancieri et al (GJI 2012)
18 Acccelerograms of the main Tocopilla earthquake 4 PBO (GFZ) stations
19 Espectro de desplazamiento del Terremoto de Tocopilla de 2007 observado en 4 estaciones de la red PBO Omega -1 Stations PB04 PB03 PB05 PB07 Moment rate 25 s From Lancieri et al (GJI 2012) and Peyrat et al (GJI 2010)
20 How to model an earthquake: Maule 27 Febrero 2010 Constitución, 19 de Marzo de 2010 Ch. Vigny
21 Central Chile Seismicity since Mw 8.3 Central Chile Mw>7.8 From Campos et al, 2002
22 Preseismic deformation from GPS «We would then conclude that the southern part of the Concepción Constitución gap has accumulated a slip deficit that is large enough to produce a very large earthquake of about Mw= » This is of course a worst case scenario that needs to be refined by additional work. (Campos, Ruegg, Vigny, R.M. et al, 2002, 2003, 2009 )
23 Ground displacement from GPS stations for themaule earthquake of 2010
24 Static GPS observation of the Maule 2010 earthquake Rupture zone 400 km Vigny et al, Science, 2011 Moreno et al, EPSL, 2012
25 Vertical displacements measured by GPS Hinge line Color diamonds Vertical displacement of biological markers (Farias et al, 2010) From Vigny et al, 2011
26 Inversion of Geodetic slip distribution Moreno et al 2012 Vigny et al 2012
27 Modelling the near field GPS data for the Mw 8.8 Maule 2010 earthquake From Vigny et al Science (2011)
28 Maule 2010: geodetic versus Far field BW inversion Slip inverted from GPS Slip Inverted from Far field body waves Mw = 8.8 Moreno et al (EPSL, 2012) Pro, Buforn, Madariaga (EGU 2013)
29 Maule 2010: Far field Body wave inversion
30 Ground velocity inversion from cgps Uses AXITRA for synthetics Ruiz Madariaga, Ruiz unpublished et al, Earthquake Spectra, 2012
31 Postseismic deformation after Maule E. Klein et al, 2015, Ruiz et al, 2015
32 Use of stacking and backprojection for modelling High frequency features
33 Low and High Frequency features of Maule 2010 Uses Backprojection 25/03/2012 Kieser and Ishii, 2011 From Ruiz et al, 2012
34 Use of seismic antennaes for stacking Source Receiver Antenna Mantle ray trajectories Rayos Frente de ondas
35 Use of a seismic receiver antenna Example of Maule aftershock Mw 7.1 of 25/3/2012 near Constitucion From SPUD in IRIS Data Center
36 Ruiz et al, EPSL 2013 Example of Maule aftershock Mw 7.1 of 25/3/2012 near Constitucion Near field Accelerogram Seismic source
37 Example of Maule aftershock Mw 7.1 of 25/3/2012 near Constitucion Far field body wave modellig
38 SH
39 Example of Maule aftershock Mw 7.1 of 25/3/2012 near Constitucion Observed and synthetic interferogram
40 Available data from the IRIS data center Wilber III applicat Red US array 25 Marzo 2012 Constitucion EQ
41 Displacement record «section» Maule aftershock Mw 7.1 of 25/3/2012 near Constitucion Traces were aligned by Cross correlation
42 Displacement record «section» Maule aftershock Mw 7.1 of 25/3/2012 near Constitucion Signal Ocean reverberations Michigan precursor Texas P sp
43 Displacement record «filter» AAM (Michigan) Maule aftershock Mw 7.1 of 25/3/2012 near Constitucion Original BB Band pass Hz Hz Hz
44 Velocity record «section» Maule aftershock Mw 7.1 of 25/3/2012 near Constitucion
45 Maule aftershock Mw 7.1 of 25/3/2012 near Constitucion 5 velocity seismograms of the US array P sp Michigan precursor Texas
46 Velocity record «filter» AAM (Michigan) Maule aftershock Mw 7.1 of 25/3/2012 near Constitucion Original BB Band pass Hz Hz Hz
47 precursor P s P Maule aftershock Mw 7.1 of 25/3/2012 near Constitucion Sum the stack at different points on the source area This is a constant latitude (-35.1) section
48 Maule aftershock Mw 7.1 of 25/3/2012 near Constitucion Sum the stack at different points on the source area This is a constant longitude (-72.03) section
49 Maule aftershock Mw 7.1 of 25/3/2012 near Constitucion This figure shows the projection (energy sum) Of the stacked seismograms
50 Use of a receiver antenna Example of Maule aftershock Mw 6.7 of 14/2/2011 near Constitucion Example of stack at different frequencies
51 Example of Maule aftershock Mw 6.7 of 14/2/2011 near Constitucion source reverberationsreve
52 Example of Maule aftershock Mw 6.7 of 14/2/2011 near Constitucion
53 There are several ways to obtain The stacked source area. Most of them are cosmetic Because at high frequency signals are coherent
54 Back Projection of Maule earthquake : Data US Array Hz Satriano et al., in progress Hz Travel time residuals corrected by multichannel cross correlation --> station corrections POLENET Array
55 Back Projection: results US Array Hz POLENET Array Hz Satriano et al., in progress
56 Teleseismic Kinematic Inversion and Back Projection US array 0-45 s s s US array POLENET array POLENET array 0-45 s s s Satriano, Donicio et al, in preparation
57 The end
Earthquake Source Dynamics and seismic radiation From large Chilean earthquakes
. Earthquake Source Dynamics and seismic radiation From large Chilean earthquakes R. Madariaga 1,2, S. Ruiz 2, F. Leyton 3, J.C. Baez 3 École Normale Supérieure de Paris, France; Centro Sismologico Nacional
More informationEarthquake stress drop estimates: What are they telling us?
Earthquake stress drop estimates: What are they telling us? Peter Shearer IGPP/SIO/U.C. San Diego October 27, 2014 SCEC Community Stress Model Workshop Lots of data for big earthquakes (rupture dimensions,
More informationEarthquake Stress Drops in Southern California
Earthquake Stress Drops in Southern California Peter Shearer IGPP/SIO/U.C. San Diego September 11, 2009 Earthquake Research Institute Lots of data for big earthquakes (rupture dimensions, slip history,
More informationSupplementary Material
1 Supplementary Material 2 3 4 Interseismic, megathrust earthquakes and seismic swarms along the Chilean subduction zone (38-18 S) 5 6 7 8 9 11 12 13 14 1 GPS data set We combined in a single data set
More informationABSTRACT. Key words: InSAR; GPS; northern Chile; subduction zone.
ASPERITIES, BARRIERS AND TRANSITION ZONE IN THE NORTH CHILE SEISMIC GAP: STATE OF THE ART AFTER THE 007 MW 7.7 TOCOPILLA EARTHQUAKE INFERRED BY GPS AND INSAR DATA Marta Bejar Pizarro, Daniel Carrizo, Anne
More informationData Repository: Seismic and Geodetic Evidence For Extensive, Long-Lived Fault Damage Zones
DR2009082 Data Repository: Seismic and Geodetic Evidence For Extensive, Long-Lived Fault Damage Zones Fault Zone Trapped Wave Data and Methods Fault zone trapped waves observed for 2 shots and 5 local
More informationJCR (2 ), JGR- (1 ) (4 ) 11, EPSL GRL BSSA
Dun Wang ( ) In collaboration with: Hitoshi Kawakatsu, Jim Mori, Kazuki Koketsu, Takuto Maeda, Hiroshi Tsuroka, Jiancang Zhunag, Lihua Fang, and Qiang Yao School of Geosciences, China University of Geosciences
More informationMechanics of Earthquakes and Faulting
Mechanics of Earthquakes and Faulting Lecture 20, 30 Nov. 2017 www.geosc.psu.edu/courses/geosc508 Seismic Spectra & Earthquake Scaling laws. Seismic Spectra & Earthquake Scaling laws. Aki, Scaling law
More informationThe 2016, October 26, Central Italy Earthquake Origin Time 17:10:36 UTC, M L(ISNet) =5.3; M W(ISNet) =5.6
The 2016, October 26, Central Italy Earthquake Origin Time 17:10:36 UTC, M L(ISNet) =5.3; M W(ISNet) =5.6 RISSC-Lab: Laboratorio di RIcerca in Sismologia Sperimentale e Computazionale The event as seen
More informationNear-Field Spectra of Large Earthquakes
Pure Appl. Geophys. Ó 2018 Springer Nature Switzerland AG https://doi.org/10.1007/s00024-018-1983-x Pure and Applied Geophysics Near-Field Spectra of Large Earthquakes RAUL MADARIAGA, 1 SERGIO RUIZ, 2
More informationMegathrust earthquakes: How large? How destructive? How often? Jean-Philippe Avouac California Institute of Technology
Megathrust earthquakes: How large? How destructive? How often? Jean-Philippe Avouac California Institute of Technology World seismicity (data source: USGS) and velocities relative to ITRF1997 (Sella et
More informationChallenges of Applying Ground Motion Simulation to Earthquake Engineering
Challenges of Applying Ground Motion Simulation to Earthquake Engineering Methodology of simulating ground motions from crustal earthquake and mega-thrust subduction earthquakes: application to the 2016
More informationData Repository of Paper: The role of subducted sediments in plate interface dynamics as constrained by Andean forearc (paleo)topography
Data Repository of Paper: The role of subducted sediments in plate interface dynamics as constrained by Andean forearc (paleo)topography Nicolás J. Cosentino 1*, Felipe Aron 2,3, Jorge G. F. Crempien 2,3,
More informationSpatio-temporal variation in slip rate on the plate boundary off Sanriku, northeastern Japan, estimated from small repeating earthquakes
Spatio-temporal variation in slip rate on the plate boundary off Sanriku, northeastern Japan, estimated from small repeating earthquakes T. Matsuzawa, N. Uchida, T. Igarashi *, N. Umino, and A. Hasegawa
More informationCase Study 2: 2014 Iquique Sequence
Case Study 2: 2014 Iquique Sequence Overview Mw 8.2 earthquake on 1 April 2014 at 11:08:43 UTC Pictures of damage Seismicity maps Foreshock seismicity -> Main shock -> Aftershock 1 April 2014 11:08:43
More informationMechanics of Earthquakes and Faulting
Mechanics of Earthquakes and Faulting Lecture 18, 16 Nov. 2017 www.geosc.psu.edu/courses/geosc508 Earthquake Magnitude and Moment Brune Stress Drop Seismic Spectra & Earthquake Scaling laws Scaling and
More informationHybrid Back-Projection: Theory and Future Direction of Seismic Array Analysis
Hybrid Back-Proection: Theory and Future Direction of Seismic Array Analysis YAGI Yui (Univ. of Tsukuba) Collaborators: FUKAHATA Yukitoshi (DPRI, Kyoto University) KASAHARA Amato, NAKAO Atsushi, EZAKI
More informationDynamic source inversion for physical parameters controlling the 2017 Lesvos earthquake
Dynamic source inversion for physical parameters controlling the 2017 Lesvos earthquake F. Kostka 1, E. Sokos 2, J. Zahradník 1, F. Gallovič 1 1 Charles University in Prague, Faculty of Mathematics and
More informationFigures S1 S4 show the measurements taken from the synthetic vespagrams where a)
Figures S1 S4 show the measurements taken from the synthetic vespagrams where a) is the differential travel time versus the Dʺ discontinuity height, b) is the differential travel time versus δv S, c) is
More informationMODELING OF HIGH-FREQUENCY WAVE RADIATION PROCESS ON THE FAULT PLANE FROM THE ENVELOPE FITTING OF ACCELERATION RECORDS
MODELING OF HIGH-FREQUENCY WAVE RADIATION PROCESS ON THE FAULT PLANE FROM THE ENVELOPE FITTING OF ACCELERATION RECORDS Yasumaro KAKEHI 1 SUMMARY High-frequency (higher than 1 Hz) wave radiation processes
More informationSOURCE MODELING OF RECENT LARGE INLAND CRUSTAL EARTHQUAKES IN JAPAN AND SOURCE CHARACTERIZATION FOR STRONG MOTION PREDICTION
SOURCE MODELING OF RECENT LARGE INLAND CRUSTAL EARTHQUAKES IN JAPAN AND SOURCE CHARACTERIZATION FOR STRONG MOTION PREDICTION Kimiyuki Asano 1 and Tomotaka Iwata 2 1 Assistant Professor, Disaster Prevention
More informationSUPPLEMENTARY INFORMATION
doi:10.1038/nature11492 Figure S1 Short-period Seismic Energy Release Pattern Imaged by F-net. (a) Locations of broadband seismograph stations in Japanese F-net used for the 0.5-2.0 Hz P wave back-projection
More informationGeodesy (InSAR, GPS, Gravity) and Big Earthquakes
Geodesy (InSAR, GPS, Gravity) and Big Earthquakes Mathew Pritchard Teh-Ru A. Song Yuri Fialko Luis Rivera Mark Simons UJNR Earthquake Research Panel, Morioka, Japan - Nov 6, 2002 Goals Accurate and high
More informationLab 9: Satellite Geodesy (35 points)
Lab 9: Satellite Geodesy (35 points) Here you will work with GPS Time Series data to explore plate motion and deformation in California. This lab modifies an exercise found here: http://www.unavco.org:8080/cws/pbonucleus/draftresources/sanandreas/
More informationPeter Shearer 1, Robin Matoza 1, Cecily Wolfe 2, Guoqing Lin 3, & Paul Okubo 4
Characterizing fault zones and volcanic conduits at Kilauea and Mauna Loa volcanoes by large-scale mapping of earthquake stress drops and high precision relocations Peter Shearer 1, Robin Matoza 1, Cecily
More informationWidespread Ground Motion Distribution Caused by Rupture Directivity during the 2015 Gorkha, Nepal Earthquake
Widespread Ground Motion Distribution Caused by Rupture Directivity during the 2015 Gorkha, Nepal Earthquake Kazuki Koketsu 1, Hiroe Miyake 2, Srinagesh Davuluri 3 and Soma Nath Sapkota 4 1. Corresponding
More informationTwo Contrasting InSAR Studies of Recent Earthquakes in Tibet
Two Contrasting InSAR Studies of Recent Earthquakes in Tibet Barry Parsons Department of Earth Sciences University of Oxford John Elliott, Wanpeng Feng,, James Jackson, Zhenhong Li, Xinjian Shan, Alastair
More informationUsing information about wave amplitudes to learn about the earthquake size.
Earthquake Magnitudes and Moments Using information about wave amplitudes to learn about the earthquake size. Need to correct for decrease with distance M = log(a/t) + F(h,Δ) + C A is the amplitude of
More informationUsing deformation rates in Northern Cascadia to constrain time-dependent stress- and slip-rate on the megathrust
Using deformation rates in Northern Cascadia to constrain time-dependent stress- and slip-rate on the megathrust Lucile Bruhat Paul Segall Stanford University 1 50 Interseismic period for the Cascadia
More informationHigh-Frequency Ground Motion Simulation Using a Source- and Site-Specific Empirical Green s Function Approach
High-Frequency Ground Motion Simulation Using a Source- and Site-Specific Empirical Green s Function Approach R. Mourhatch & S. Krishnan California Institute of Technology, Pasadena, CA, USA SUMMARY: A
More informationSeth Stein and Emile Okal, Department of Geological Sciences, Northwestern University, Evanston IL USA. Revised 2/5/05
Sumatra earthquake moment from normal modes 2/6/05 1 Ultra-long period seismic moment of the great December 26, 2004 Sumatra earthquake and implications for the slip process Seth Stein and Emile Okal,
More informationForearc deformation across time scales - a tale of fluids, locking and transients
Forearc deformation across time scales - a tale of fluids, locking and transients Modified from Scholz, 1998; Bilek & Lay, 2002; and Schwartz & Rokosky, 2007 Onno Oncken, GFZ Potsdam with M. Moreno, P.
More informationImaging short-period seismic radiation from the 27 February 2010 Chile (M W 8.8) earthquake by back-projection of P, PP, and PKIKP waves
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 117,, doi:10.1029/2011jb008576, 2012 Imaging short-period seismic radiation from the 27 February 2010 Chile (M W 8.8) earthquake by back-projection of P, PP, and PKIKP
More informationSeismogeodesy for rapid earthquake and tsunami characterization
Seismogeodesy for rapid earthquake and tsunami characterization Yehuda Bock Scripps Orbit and Permanent Array Center Scripps Institution of Oceanography READI & NOAA-NASA Tsunami Early Warning Projects
More information5th Workshop on "SMART Cable Systems: Latest Developments and Designing the Wet Demonstrator Project"
5th Workshop on "SMART Cable Systems: Latest Developments and Designing the Wet Demonstrator Project" (Dubai, UAE, 17-18 April 2016) Benefits and requirements for ocean bottom measurements for tsunami
More informationSeismic slip on an upper-plate normal fault during a large subduction megathrust rupture
SUPPLEMENTARY INFORMATION DOI: 10.1038/NGEO2585 Seismic slip on an upper-plate normal fault during a large subduction megathrust rupture Stephen P. Hicks* and Andreas Rietbrock NATURE GEOSCIENCE www.nature.com/naturegeoscience
More informationJournalofGeophysicalResearch: SolidEarth
JournalofGeophysicalResearch: SolidEarth RESEARCH ARTICLE Key Points: Relations between source dimensions and corner frequencies are established Stress drop estimates are affected by differences in source
More informationSelected Seismic Observations of Upper-Mantle Discontinuities
Selected Seismic Observations of Upper-Mantle Discontinuities Peter Shearer IGPP/SIO/U.C. San Diego August 31, 2009 Earthquake Research Institute Interface Depth vs. Publication Date Most depths are sampled
More informationVertical to Horizontal (V/H) Ratios for Large Megathrust Subduction Zone Earthquakes
Vertical to Horizontal (V/H) Ratios for Large Megathrust Subduction Zone Earthquakes N.J. Gregor Consultant, Oakland, California, USA N.A. Abrahamson University of California, Berkeley, USA K.O. Addo BC
More informationBROADBAND STRONG MOTION SIMULATION OF THE 2004 NIIGATA- KEN CHUETSU EARTHQUAKE: SOURCE AND SITE EFFECTS
Third International Symposium on the Effects of Surface Geology on Seismic Motion Grenoble, France, 30 August - 1 September 2006 Paper Number: 105 BROADBAND STRONG MOTION SIMULATION OF THE 2004 NIIGATA-
More informationMagnitude 7.8 SCOTIA SEA
A magnitude 7.8 earthquake has occurred in the South Orkney Island region in the Scotia Sea. According to the USGS, this earthquake is the latest in a series of moderate-tolarge earthquakes to strike this
More informationMagnitude 8.2 NORTHWEST OF IQUIQUE, CHILE
An 8.2-magnitude earthquake struck off the coast of northern Chile, generating a local tsunami. The USGS reported the earthquake was centered 95 km (59 miles) northwest of Iquique at a depth of 20.1km
More informationRegional Geodesy. Shimon Wdowinski. MARGINS-RCL Workshop Lithospheric Rupture in the Gulf of California Salton Trough Region. University of Miami
MARGINS-RCL Workshop Lithospheric Rupture in the Gulf of California Salton Trough Region Regional Geodesy Shimon Wdowinski University of Miami Rowena Lohman, Kim Outerbridge, Tom Rockwell, and Gina Schmalze
More informationThe Earthquake of Padang, Sumatra of 30 September 2009 scientific information and update
The Earthquake of Padang, Sumatra of 30 September 2009 scientific information and update 01-October-2009 Christophe Vigny Directeur de recherches at CNRS Laboratoire de Géologie Geoscience Dept. Of ENS,
More informationSection Forces Within Earth. 8 th Grade Earth & Space Science - Class Notes
Section 19.1 - Forces Within Earth 8 th Grade Earth & Space Science - Class Notes Stress and Strain Stress - is the total force acting on crustal rocks per unit of area (cause) Strain deformation of materials
More informationModelling Strong Ground Motions for Subduction Events in the Wellington Region, New Zealand
Proceedings of the Ninth Pacific Conference on Earthquake Engineering Building an Earthquake-Resilient Society 14-16 April, 2011, Auckland, New Zealand Modelling Strong Ground Motions for Subduction Events
More informationCase Study 1: 2014 Chiang Rai Sequence
Case Study 1: 2014 Chiang Rai Sequence Overview Mw 6.1 earthquake on 5 May 2014 at 11:08:43 UTC Largest recorded earthquake in Thailand Fault Orientation How does the orientation of the fault affect the
More informationEARTHQUAKE SOURCE PARAMETERS OF MODERATELY EARTHQUAKE IN THE SOUTH EASTERN IRAN BASED ON TELESEISMIC AND REGIONAL DISTANCES
EARTHQUAKE SOURCE PARAMETERS OF MODERATELY EARTHQUAKE IN THE SOUTH EASTERN IRAN BASED ON TELESEISMIC AND REGIONAL DISTANCES M. Mostafazadeh 1 and S.Ashkpour Motlagh 2 1 Assistant Professor,Seismology Research
More informationOVERVIEW INTRODUCTION 3 WHAT'S MISSING? 4 OBJECTIVES 5
OVERVIEW INTRODUCTION 3 WHAT'S MISSING? 4 OBJECTIVES 5 DISTORTION OF SEISMIC SOURCE SPECTRUM 6 PRINCIPLE 7 SEISMIC SOURCE SPECTRUM 8 EFFECT OF RECORDING INSTRUMENTS 9 SEISMOMETERS 9 CORRECTION FOR FREQUENCY
More informationThe Earthquake Cycle Chapter :: n/a
The Earthquake Cycle Chapter :: n/a A German seismogram of the 1906 SF EQ Image courtesy of San Francisco Public Library Stages of the Earthquake Cycle The Earthquake cycle is split into several distinct
More informationEarthquake Source. Kazuki Koketsu. Special Session: Great East Japan (Tohoku) Earthquake. Earthquake Research Institute, University of Tokyo
2012/9/24 17:20-17:35 WCEE SS24.4 Special Session: Great East Japan (Tohoku) Earthquake Earthquake Source Kazuki Koketsu Earthquake Research Institute, University of Tokyo 1 Names and features of the earthquake
More informationSimulation of earthquake rupture process and strong ground motion
Simulation of earthquake rupture process and strong ground motion Takashi Miyatake (1) and Tomohiro Inoue (2) (1) Earthquake Research Institute, University of Tokyo, Yayoi, Bunkyo, Tokyo, 113-0032, Japan
More informationNew Prediction Formula of Fourier Spectra Based on Separation Method of Source, Path, and Site Effects Applied to the Observed Data in Japan
New Prediction Formula of Fourier Spectra Based on Separation Method of Source, Path, and Site Effects Applied to the Observed Data in Japan Kenichi Nakano Graduate School of Engineering, Kyoto University,
More informationEmpirical Green s Function Analysis of the Wells, Nevada, Earthquake Source
Nevada Bureau of Mines and Geology Special Publication 36 Empirical Green s Function Analysis of the Wells, Nevada, Earthquake Source by Mendoza, C. 1 and Hartzell S. 2 1 Centro de Geociencias, Universidad
More informationIncorporating simulated Hikurangi subduction interface spectra into probabilistic hazard calculations for Wellington
Incorporating simulated Hikurangi subduction interface spectra into probabilistic hazard calculations for Wellington G.H. McVerry & C. Holden GNS Science, Lower Hutt, New Zealand. 2014 NZSEE Conference
More informationIntroduction to Displacement Modeling
Introduction to Displacement Modeling Introduction Deformation on the Earth surface informs us about processes and material properties below surface Observation tools: GPS (static-dynamic) InSAR (static)
More informationMMA Memo No National Radio Astronomy Observatory. Seismicity and Seismic Hazard at MMA site, Antofagasta, Chile SERGIO E.
MMA Memo No. 250 National Radio Astronomy Observatory Seismicity and Seismic Hazard at MMA site, Antofagasta, Chile SERGIO E. BARRIENTOS Departamento de Geofisica Universidad de Chile June, 1996 Seismicity
More informationOriginally published as:
Originally published as: Lange, D., Bedford, J., Moreno, M., Tilmann, F., Baez, J. C., Bevis, M., Kruger, F. (2014): Comparison of postseismic afterslip models with aftershock seismicity for three subduction-zone
More informationStrong Ground Motion Attenuation Relations for Chilean Subduction Zone Interface Earthquakes
Strong Ground Motion Attenuation Relations for Chilean Subduction Zone Interface Earthquakes V. Contreras & R. Boroschek Department of Civil Engineering, University of Chile, Chile SUMMARY: Attenuation
More informationScientific Research on the Cascadia Subduction Zone that Will Help Improve Seismic Hazard Maps, Building Codes, and Other Risk-Mitigation Measures
Scientific Research on the Cascadia Subduction Zone that Will Help Improve Seismic Hazard Maps, Building Codes, and Other Risk-Mitigation Measures Art Frankel U.S. Geological Survey Seattle, WA GeoPrisms-Earthscope
More informationShort-Period Rupture Process of the 2010 M w 8.8 Maule Earthquake in Chile
Short-Period Rupture Process of the 21 M w 8.8 Maule Earthquake in Chile Sergio Ruiz, a), b) Raúl Madariaga, a) Maximiliano Astroza, c) G. Rodolfo Saragoni, c) María Lancieri, d) Christophe Vigny, a) and
More informationKinematics of the Southern California Fault System Constrained by GPS Measurements
Title Page Kinematics of the Southern California Fault System Constrained by GPS Measurements Brendan Meade and Bradford Hager Three basic questions Large historical earthquakes One basic question How
More informationMegathrust Earthquakes
Megathrust Earthquakes Susan Schwartz University of California Santa Cruz CIDER 2017 UC Berkeley July 5, 2017 The largest megathrust events are not uniformally distributed at all subduction zones. M>8
More informationToday: Basic regional framework. Western U.S. setting Eastern California Shear Zone (ECSZ) 1992 Landers EQ 1999 Hector Mine EQ Fault structure
Today: Basic regional framework Western U.S. setting Eastern California Shear Zone (ECSZ) 1992 Landers EQ 1999 Hector Mine EQ Fault structure 1 2 Mojave and Southern Basin and Range - distribution of strike-slip
More informationA GLOBAL SURGE OF GREAT EARTHQUAKES AND WHAT WE ARE LEARNING FROM THEM. Thorne Lay, University of California Santa Cruz
A GLOBAL SURGE OF GREAT EARTHQUAKES AND WHAT WE ARE LEARNING FROM THEM Thorne Lay, University of California Santa Cruz Plate boundaries are a planet-wide network of faults where most earthquakes and volcanoes
More informationSource parameters II. Stress drop determination Energy balance Seismic energy and seismic efficiency The heat flow paradox Apparent stress drop
Source parameters II Stress drop determination Energy balance Seismic energy and seismic efficiency The heat flow paradox Apparent stress drop Source parameters II: use of empirical Green function for
More informationDistribution of slip from 11 M w > 6 earthquakes in the northern Chile subduction zone
Click Here for Full Article JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 111,, doi:10.1029/2005jb004013, 2006 Distribution of slip from 11 M w > 6 earthquakes in the northern Chile subduction zone M. E. Pritchard,
More informationMagnitude Area Scaling of SCR Earthquakes. Summary
Magnitude Area Scaling of SCR Earthquakes Paul Somerville Summary Review of Existing Models Description of New Model Comparison of New and Existing Models Existing Models Allman & Shearer, 2009 Global,
More informationI. Locations of Earthquakes. Announcements. Earthquakes Ch. 5. video Northridge, California earthquake, lecture on Chapter 5 Earthquakes!
51-100-21 Environmental Geology Summer 2006 Tuesday & Thursday 6-9:20 p.m. Dr. Beyer Earthquakes Ch. 5 I. Locations of Earthquakes II. Earthquake Processes III. Effects of Earthquakes IV. Earthquake Risk
More informationJoint inversion of InSAR and broadband teleseismic waveform data with ABIC: application to the 1997 Manyi, Tibet earthquake
Joint inversion of InSAR and broadband teleseismic waveform data with ABIC: application to the 1997 Manyi, Tibet earthquake Gareth Funning 1, Yukitoshi Fukahata 2, Yuji Yagi 3 & Barry Parsons 4 1 University
More informationDeveloping ENA GMPE s Using Broadband Synthe=c Seismograms from Finite- Fault Simula=ons
Developing ENA GMPE s Using Broadband Synthe=c Seismograms from Finite- Fault Simula=ons Art Frankel U.S. Geological Survey SeaFle, WA NGA- East workshop Oct 29, 2014 From Frankel (2009) 1 ENA broadband
More informationRegional deformation and kinematics from GPS data
Regional deformation and kinematics from GPS data Jessica Murray, Jerry Svarc, Elizabeth Hearn, and Wayne Thatcher U. S. Geological Survey Acknowledgements: Rob McCaffrey, Portland State University UCERF3
More informationInversion of Earthquake Rupture Process:Theory and Applications
Inversion of Earthquake Rupture Process:Theory and Applications Yun-tai CHEN 12 * Yong ZHANG 12 Li-sheng XU 2 1School of the Earth and Space Sciences, Peking University, Beijing 100871 2Institute of Geophysics,
More informationPUBLICATIONS. Journal of Geophysical Research: Solid Earth
PUBLICATIONS Journal of Geophysical Research: Solid Earth RESEARCH ARTICLE Key Points: Frequency dependence of directivity is observed at UPSAR for the 2004 Parkfield earthquake Seismic radiation from
More informationOutstanding Problems. APOSTOLOS S. PAPAGEORGIOU University of Patras
NEAR-FAULT GROUND MOTIONS: Outstanding Problems APOSTOLOS S. PAPAGEORGIOU University of Patras Outline Characteristics of near-fault ground motions Near-fault strong ground motion database A mathematical
More informationGeotechnical Earthquake Engineering
Geotechnical Earthquake Engineering by Dr. Deepankar Choudhury Professor Department of Civil Engineering IIT Bombay, Powai, Mumbai 400 076, India. Email: dc@civil.iitb.ac.in URL: http://www.civil.iitb.ac.in/~dc/
More informationSOURCE PROCESS OF THE 2003 PUERTO PLATA EARTHQUAKE USING TELESEISMIC DATA AND STRONG GROUND MOTION SIMULATION
Synopses of Master Papers Bulletin of IISEE, 47, 19-24, 2013 SOURCE PROCESS OF THE 2003 PUERTO PLATA EARTHQUAKE USING TELESEISMIC DATA AND STRONG GROUND MOTION SIMULATION Fabricio Moquete Everth* Supervisor:
More information12/07/2013. Apparent sea level rise and earthquakes
Main collaborations: - P. Simeoni - M. N. Bouin - S. Calmant Valérie Ballu Valerie.ballu@univ-lr.fr Apparent sea level rise and earthquakes possibly the world s first community to be formally moved out
More informationOriginally published as:
Originally published as: Lorenzo Martín, F., Wang, R., Roth, F. (2002): The effect of input parameters on visco-elastic models of crustal deformation. - Física de la Tierra, 14, 33-54 The effect of input
More informationEARTH STRUCTURE & DYNAMICS EARTHQUAKE SEISMOLOGY PRACTICALS. G.R. Foulger
1 EARTH STRUCTURE & DYNAMICS EARTHQUAKE SEISMOLOGY PRACTICALS G.R. Foulger 1. A large earthquake is recorded well at a three-component seismic station in Hawaii (coordinates 205 E, 20 N). The epicentral
More informationTitle. Author(s)Heki, Kosuke. CitationScience, 332(6036): Issue Date Doc URL. Type. File Information. A Tale of Two Earthquakes
Title A Tale of Two Earthquakes Author(s)Heki, Kosuke CitationScience, 332(6036): 1390-1391 Issue Date 2011-06-17 Doc URL http://hdl.handle.net/2115/48524 Type article (author version) File Information
More informationSendai Earthquake NE Japan March 11, Some explanatory slides Bob Stern, Dave Scholl, others updated March
Sendai Earthquake NE Japan March 11, 2011 Some explanatory slides Bob Stern, Dave Scholl, others updated March 14 2011 Earth has 11 large plates and many more smaller ones. Plates are 100-200 km thick
More informationKeywords: Drab-e-Astane earthquake, Empirical green's function, Kostrov slip function, Simulation.
Synthesizing the 2006 Silakhor (Darb-e-Astane) earthquake (Iran), using Empirical Green s function method A. Nicknam, R. Abbasnia, Y. Eslamian, M. Bozorgnasab, fariborz Nicknam, M.A.Sadredini 1. Assistant
More informationRECIPE FOR PREDICTING STRONG GROUND MOTIONS FROM FUTURE LARGE INTRASLAB EARTHQUAKES
RECIPE FOR PREDICTING STRONG GROUND MOTIONS FROM FUTURE LARGE INTRASLAB EARTHQUAKES T. Sasatani 1, S. Noguchi, T. Maeda 3, and N. Morikawa 4 1 Professor, Graduate School of Engineering, Hokkaido University,
More informationEnhancement of Earthquake and Tsunami Disaster Mitigation Technology in Peru
Science and Technology Research Partnership for Sustainable Development (SATREPS) Enhancement of Earthquake and Tsunami Disaster Mitigation Technology in Peru PROGRESS OF THE PROJECT 213 G1 GROUP (Seismic
More informationSupplementary Materials for
advances.sciencemag.org/cgi/content/full/4/3/eaao4915/dc1 Supplementary Materials for Global variations of large megathrust earthquake rupture characteristics This PDF file includes: Lingling Ye, Hiroo
More informationJournal of Geophysical Research (Solid Earth) Supporting Information for
Journal of Geophysical Research (Solid Earth) Supporting Information for Postseismic Relocking of the Subduction Megathrust Following the 2007 Pisco, Peru earthquake D.Remy (a), H.Perfettini (b), N.Cotte
More informationQuiz 6. 1) The measure of the time between two peaks of a sine wave is called the. A) period B) wavelength C) amplitude.
Quiz 6 1) The measure of the time between two peaks of a sine wave is called the A) period B) wavelength C) amplitude Amplitude (m) Motion of one point Time (s) Hint: look at the units of the axis. Quiz
More informationby Bertrand Delouis, Mario Pardo, Denis Legrand, * and Tony Monfret Introduction
Bulletin of the Seismological Society of America, Vol. 99, No. 1, pp. 87 94, February 2009, doi: 10.1785/0120080192 The M w 7.7 Tocopilla Earthquake of 14 November 2007 at the Southern Edge of the Northern
More informationoverlie the seismogenic zone offshore Costa Rica, making the margin particularly well suited for combined land and ocean geophysical studies (Figure
Chapter 1 Introduction Historically, highly destructive large magnitude (M w >7.0) underthrusting earthquakes nucleate along the shallow segment of subduction zone megathrust fault, and this region of
More informationSeismic Source Mechanism
Seismic Source Mechanism Yuji Yagi (University of Tsukuba) Earthquake Earthquake is a term used to describe both failure process along a fault zone, and the resulting ground shaking and radiated seismic
More informationImaging sharp lateral velocity gradients using scattered waves on dense arrays: faults and basin edges
2017 SCEC Proposal Report #17133 Imaging sharp lateral velocity gradients using scattered waves on dense arrays: faults and basin edges Principal Investigator Zhongwen Zhan Seismological Laboratory, California
More informationSTUDYING THE IMPORTANT PARAMETERS IN EARTHQUAKE SIMULATION BASED ON STOCHASTIC FINITE FAULT MODELING
STUDYING THE IMPORTANT PARAMETERS IN EARTHQUAKE SIMULATION BASED ON STOCHASTIC FINITE FAULT MODELING H. Moghaddam 1, N. Fanaie 2* and H. Hamzehloo 1 Professor, Dept. of civil Engineering, Sharif University
More informationJournal of Geophysical Research Letters Supporting Information for
Journal of Geophysical Research Letters Supporting Information for InSAR observations of strain accumulation and fault creep along the Chaman Fault system, Pakistan and Afghanistan H. Fattahi 1, F. Amelung
More informationEarthquake Engineering GE / CE - 479/679
Earthquake Engineering GE / CE - 479/679 Topic 4. Seismometry John G. Anderson Director February 4-6, 2003 1 Wood-Anderson Seismograph Important because: Principles of operation are widely used. Basis
More information27th Seismic Research Review: Ground-Based Nuclear Explosion Monitoring Technologies
SEISMIC SOURCE AND PATH CALIBRATION IN THE KOREAN PENINSULA, YELLOW SEA, AND NORTHEAST CHINA Robert B. Herrmann 1, Young-Soo Jeon 1, William R. Walter 2, and Michael E. Pasyanos 2 Saint Louis University
More informationBasics of the modelling of the ground deformations produced by an earthquake. EO Summer School 2014 Frascati August 13 Pierre Briole
Basics of the modelling of the ground deformations produced by an earthquake EO Summer School 2014 Frascati August 13 Pierre Briole Content Earthquakes and faults Examples of SAR interferograms of earthquakes
More informationSeismic-afterslip characterization of the 2010 M W 8.8 Maule, Chile, earthquake based on moment tensor inversion
GEOPHYSICAL RESEARCH LETTERS, VOL. 39,, doi:10.1029/2012gl053434, 2012 Seismic-afterslip characterization of the 2010 M W 8.8 Maule, Chile, earthquake based on moment tensor inversion Hans Agurto, 1 Andreas
More informationTechnical Report December 25, 2016, Mw=7.6, Chiloé Earthquake
Technical Report December 25, 2016, Mw=7.6, Chiloé Earthquake Sergio Barrientos and the CSN team On December 25, 2016 at 11:22 a.m. (local time) an Mw=7.6 earthquake took place on the coast of the Los
More information27th Seismic Research Review: Ground-Based Nuclear Explosion Monitoring Technologies
GROUND TRUTH LOCATIONS USING SYNERGY BETWEEN REMOTE SENSING AND SEISMIC METHODS-APPLICATION TO CHINESE AND NORTH AFRICAN EARTHQUAKES C. K. Saikia 1, H. K. Thio 2, D. V. Helmberger 2, G. Ichinose 1, and
More information