Tracking Earthquake Cascades

Total Page:16

File Type:pdf, Size:1020Kb

Tracking Earthquake Cascades The Southern California Earthquake Center, Phase 4 (SCEC4): Tracking Earthquake Cascades Proposal Submitted to National Science Foundation and U.S. Geological Survey March 2010 Project Summary.............................................................................................................i I. Introduction...............................................................................................................1 A. Southern California as a Natural Laboratory...................................................................... 1 B. SCEC as a Virtual Organization......................................................................................... 3 C. Earthquake System Science .............................................................................................. 5 D. Intellectual Merit of the Proposed Research ...................................................................... 5 E. Broader Impacts of the Proposed Research ...................................................................... 6 II. Research Accomplishments....................................................................................7 A. Science Accomplishments ................................................................................................. 7 1. Develop the Unified Structural Representation ............................................................ 8 2. Develop an Extended Earthquake Rupture Forecast................................................. 10 3. Predict Broadband Ground Motions ........................................................................... 17 4. Prepare Post-Earthquake Scientific Response Strategies ......................................... 20 B. Communication, Education & Outreach Accomplishments.............................................. 21 1. 2009 Program Evaluation........................................................................................... 21 2. Major Activities and Results ....................................................................................... 21 C. Information Technology Accomplishments....................................................................... 25 III. SCEC4 Project Plan ................................................................................................27 A. SCEC4 Vision Statement ................................................................................................. 27 B. Science Plan .................................................................................................................... 28 1. Fundamental Problems of Earthquake Physics ......................................................... 29 2. Interdisciplinary Research Initiatives .......................................................................... 41 2. System-Science Challenges and SCEC4 Organization ............................................. 44 C. Communication, Education & Outreach Plan................................................................... 47 1. Implementation Interface............................................................................................ 48 2. Public Education and Preparedness .......................................................................... 49 3. K-14 Earthquake Education Initiative ......................................................................... 51 4. Experiential Learning and Career Advancement........................................................ 52 D. Diversity Plan ................................................................................................................... 53 E. Information Technology Plan............................................................................................ 54 IV. Management Plan ...................................................................................................56 A. Organization of the Center ............................................................................................... 56 B. Budgeting Process ........................................................................................................... 58 C. Operations Following a Major Earthquake ....................................................................... 59 V. References ..............................................................................................................61 Project Summary This proposal requests funding for the Southern California Earthquake Center (SCEC) for the 5-year period from 1 Feb 2012 to 31 Jan 2017 (SCEC4). The Center coordinates basic research in earthquake science using Southern California as its principal natural laboratory. The region is data-rich and, with an urbanized population exceeding 20 million, it comprises the lion’s share of national earthquake risk. Ac- cording to the Uniform California Earthquake Rupture Forecast (UCERF2), the mean probability of an M > 7 earthquake in Southern California over the next 30 years is 82%. New research by the Southern San Andreas Fault Evaluation (SoSAFE) project has revised the recurrence interval for the Carrizo sec- tion of the San Andreas fault downward, to less than the open interval since its last rupture in 1857. The entire southern San Andreas is “locked and loaded.” SCEC Mission. SCEC’s theme of earthquake system science is reflected in its mission statement, which emphasizes the connections between information gathering by sensor networks, fieldwork, and laboratory experiments; knowledge formulation through physics-based, system-level modeling; improved under- standing of seismic hazard; and actions to reduce earthquake risk and promote community resilience. The Center is a large consortium of institutions with a national, and increasingly worldwide, distribution that coordinates earthquake system science within Southern California, and with research elsewhere. The 16 current core institutions have all committed resources to SCEC4, and three new core institutions are expected to join, including a consortium of 6 CalState campuses. More than 50 other institutions (11 for- eign) are likely to participate, forming one of the largest research collaborations in geoscience. Several other characteristics describe the Center: - A collaboratory for earthquake system science that includes the Community Modeling Environ- ment (CME), which applies high-performance computing to large-scale earthquake modeling, and the Collaboratory for the Study of Earthquake Predictability (CSEP), a global infrastructure for the prospective testing of earthquake forecasts. - An open “community of trust” that nurtures stu- dents and early-career scientists and shares in- formation and ideas about how earthquakes work. The Center’s working groups, workshops, field ac- tivities, and annual meeting enable scientists to collaborate over sustained periods, building strong interpersonal networks that promote intellectual exchange and mutual support. About two-thirds of the total SCEC science budget directly supports students and early-career scientists (Fig. S1). - A reliable and trusted partner that collaborates with other organizations in reducing risk and pro- moting societal resilience to earthquake disasters. The SCEC Communication, Education, and Out- reach (CEO) program has steadily grown a di- verse network of partnerships. Its California-wide Earthquake Country Alliance (ECA)—now compris- ing more than 200 organizations—promotes preparedness through the popular publications that have branched from Putting Down Roots in Earthquake Country and involves millions of California citizens in earthquake awareness and readiness exercises through its annual ShakeOut exercises. Intellectual Merit of the Proposed Research. Earthquakes emerge from complex, multiscale interac- tions within active fault systems that are opaque, and are thus difficult to observe. They cascade as cha- otic chain reactions through the natural and built environments, and are thus difficult to predict. The pro- posed 5-year research program will pioneer time-dependent seismic hazard analysis—the geoscience required to track earthquake cascades. This science seeks to understand the unusual physics of how i matter and energy interact during the extreme conditions of rock failure. No theory adequately describes the basic features of dynamic rupture, nor is one available that fully explains the dynamical interactions within networks of faults. Progress towards a comprehensive theory will improve the predictive capabili- ties of earthquake system science. SCEC4 will move this science forward through highly integrated collaborations that are coordinated across scientific disciplines and research institutions and enabled by high-performance computing and advanced information technology. It will focus on six fundamental problems of earthquake physics: a. Stress transfer from plate motion to crustal faults: long-term fault slip rates. b. Stress-mediated fault interactions and earthquake clustering: evaluation of mechanisms. c. Evolution of fault resistance during seismic slip: scale-appropriate laws for rupture modeling. d. Structure and evolution of fault zones and systems: relation to earthquake physics. e. Causes and effects of transient deformations: slow slip events and tectonic tremor. f. Seismic wave generation and scattering: prediction of strong ground motions. Broader Impacts of the Proposed Research. The Center will translate basic research into practical products for reducing risk and improving community resilience in Southern California and elsewhere. The SCEC4 program will help to: - transform
Recommended publications
  • The 2018 Mw 7.5 Palu Earthquake: a Supershear Rupture Event Constrained by Insar and Broadband Regional Seismograms
    remote sensing Article The 2018 Mw 7.5 Palu Earthquake: A Supershear Rupture Event Constrained by InSAR and Broadband Regional Seismograms Jin Fang 1, Caijun Xu 1,2,3,* , Yangmao Wen 1,2,3 , Shuai Wang 1, Guangyu Xu 1, Yingwen Zhao 1 and Lei Yi 4,5 1 School of Geodesy and Geomatics, Wuhan University, Wuhan 430079, China; [email protected] (J.F.); [email protected] (Y.W.); [email protected] (S.W.); [email protected] (G.X.); [email protected] (Y.Z.) 2 Key Laboratory of Geospace Environment and Geodesy, Ministry of Education, Wuhan University, Wuhan 430079, China 3 Collaborative Innovation Center of Geospatial Technology, Wuhan University, Wuhan 430079, China 4 Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China; [email protected] 5 Qinghai Provincial Key Laboratory of Geology and Environment of Salt Lakes, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China * Correspondence: [email protected]; Tel.: +86-27-6877-8805 Received: 4 April 2019; Accepted: 29 May 2019; Published: 3 June 2019 Abstract: The 28 September 2018 Mw 7.5 Palu earthquake occurred at a triple junction zone where the Philippine Sea, Australian, and Sunda plates are convergent. Here, we utilized Advanced Land Observing Satellite-2 (ALOS-2) interferometry synthetic aperture radar (InSAR) data together with broadband regional seismograms to investigate the source geometry and rupture kinematics of this earthquake. Results showed that the 2018 Palu earthquake ruptured a fault plane with a relatively steep dip angle of ~85◦.
    [Show full text]
  • Notice This Manuscript Is a Non-Peer Reviewed Preprint Submitted To
    Notice This manuscript is a non-peer reviewed preprint submitted to EarthArXiv. It has been submitted for publication to GRL on 01/10/2019 with reference number #2019GL085649. Newer versions may be moderately different with slight variations in content. Manuscript details Title: Does a damaged-fault zone mitigate the near-field impact of supershear earthquakes?—Application to the 2018 Mw 7.5 Palu earthquake Authors: Elif Oral, Huihui Weng and Jean-Paul Ampuero Contact: [email protected] manuscript submitted to Geophysical Research Letters 1 Does a damaged-fault zone mitigate the near-field 2 impact of supershear earthquakes?—Application to the 3 2018 Mw 7.5 Palu earthquake 1 1 1,2 4 Elif Oral , Huihui Weng , and Jean Paul Ampuero 1 5 Universit´eCˆote d’Azur, IRD, CNRS, Observatoire de la Cˆote d’Azur, G´eoazur, France 2 6 California Institute of Technology, Seismological Laboratory, Pasadena, CA, USA 7 Key Points: 8 • The unexpectedly low rupture speed of the 2018 Palu supershear earthquake can 9 be explained by a fault damage zone. 10 • The reduction of rupture speed by a fault damage zone mitigates the near-field 11 ground motion and landslide hazard. 12 • Fault zone waves amplify ground motions, but not enough to compensate for the 13 mitigation e↵ect of rupture speed. Corresponding author: Elif Oral, [email protected] –1– manuscript submitted to Geophysical Research Letters 14 Abstract 15 The impact of earthquakes can be severely aggravated by cascading secondary hazards. 16 The 2018 Mw 7.5 Palu, Indonesia earthquake led to devastating tsunamis and landslides, 17 while triggered submarine landslides possibly contributed substantially to generate the 18 tsunami.
    [Show full text]
  • Coherence of Mach Fronts During Heterogeneous Supershear Earthquake Rupture Propagation: Simulations and Comparison with Observations A
    JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 115, B08301, doi:10.1029/2009JB006819, 2010 Coherence of Mach fronts during heterogeneous supershear earthquake rupture propagation: Simulations and comparison with observations A. Bizzarri,1 Eric M. Dunham,2,3 and P. Spudich4 Received 24 July 2009; revised 18 February 2010; accepted 25 February 2010; published 3 August 2010. [1] We study how heterogeneous rupture propagation affects the coherence of shear and Rayleigh Mach wavefronts radiated by supershear earthquakes. We address this question using numerical simulations of ruptures on a planar, vertical strike‐slip fault embedded in a three‐dimensional, homogeneous, linear elastic half‐space. Ruptures propagate spontaneously in accordance with a linear slip‐weakening friction law through both homogeneous and heterogeneous initial shear stress fields. In the 3‐D homogeneous case, rupture fronts are curved owing to interactions with the free surface and the finite fault width; however, this curvature does not greatly diminish the coherence of Mach fronts relative to cases in which the rupture front is constrained to be straight, as studied by Dunham and Bhat (2008a). Introducing heterogeneity in the initial shear stress distribution causes ruptures to propagate at speeds that locally fluctuate above and below the shear wave speed. Calculations of the Fourier amplitude spectra (FAS) of ground velocity time histories corroborate the kinematic results of Bizzarri and Spudich (2008a): (1) The ground motion of a supershear rupture is richer in high frequency with respect to a subshear one. (2) When a Mach pulse is present, its high frequency content overwhelms that arising from stress heterogeneity. Present numerical experiments indicate that a Mach pulse causes approximately an w−1.7 high frequency falloff in the FAS of ground displacement.
    [Show full text]
  • Laboratory Earthquakes
    International Journal of Fracture (2006) 138:211–218 DOI 10.1007/s10704-006-0030-6 © Springer 2006 Laboratory earthquakes ARES J. ROSAKIS1,∗, HIROO KANAMORI2 and KAIWEN XIA3 1Graduate Aeronautical Laboratories, California Institute of Technology, Pasadena, CA 91125, USA 2Seismological Laboratory, California Institute of Technology, Pasadena, CA 91125, USA 3Department of Civil Engineering, University of Toronto, 35 St. George Street, Toronto, ON M5S 1A4, Canada ∗Author for correspondence (E-mail: [email protected]) Received 1 March 2005; accepted 1 December 2005 Abstract. We report on the experimental observation of the phenomenon of, spontaneously nucleated, supershear rupture and on the visualization of the mechanism of subRayleigh to supershear rupture transition in frictionally-held interfaces. The laboratory experiments mimic natural earthquakes. The results suggest that under certain conditions supershear rupture propagation can be facilitated during large earthquakes. Key words: Earthquake rupture, supershear, subRayleigh, transition. 1. Introduction Vertically dipping crustal faults are long pre-existing weak planes that extend tens of kilometers perpendicularly to the earth’s surface and often host catastrophic earth- quake rupture events. The geometry (planarity and length) of such faults is often sim- ple enough to apply appropriately modified concepts of dynamic fracture mechanics to the study of the physics underlying their rupture process. Due to the nature of earthquakes however, direct full field and real time observations of the rupture pro- cess are prohibited while even strong motion data have limitations of spatial resolu- tion. As a result, most efforts to date have focused on complicated analytical studies and on extensive numerical modeling of dynamic rupture processes using finite ele- ment, finite difference, and boundary element methods.
    [Show full text]
  • Observation of Far-Field Mach Waves Generated by the 2001 Kokoxili Supershear Earthquake, M
    Observation of far-field Mach waves generated by the 2001 Kokoxili supershear earthquake, M. Vallée, E.M. Dunham To cite this version: M. Vallée, E.M. Dunham. Observation of far-field Mach waves generated by the 2001 Kokoxili su- pershear earthquake,. Geophysical Research Letters, American Geophysical Union, 2012, 39 (5), pp.L05311. 10.1029/2011GL050725. hal-01053146 HAL Id: hal-01053146 https://hal.archives-ouvertes.fr/hal-01053146 Submitted on 19 May 2017 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. GEOPHYSICAL RESEARCH LETTERS, VOL. 39, L05311, doi:10.1029/2011GL050725, 2012 Observation of far-field Mach waves generated by the 2001 Kokoxili supershear earthquake M. Vallée1 and Eric M. Dunham2 Received 21 December 2011; revised 13 February 2012; accepted 13 February 2012; published 14 March 2012. [1] Regional surface wave observations offer a powerful Dunham and Archuleta, 2004; Aagaard and Heaton, 2004; tool for determining source properties of large earthquakes, Robinson et al., 2006; Vallée et al., 2008; Walker and especially rupture velocity. Supershear ruptures, being Shearer, 2009]. faster than surface wave phase velocities, create far-field [3] The most distinctive features of supershear ruptures surface wave Mach cones along which waves from all are Mach fronts.
    [Show full text]
  • Supershear Rupture in the 24 May 2013 Mw 6.7 Okhotsk Deep
    PUBLICATIONS Geophysical Research Letters RESEARCH LETTER Supershear rupture in the 24 May 2013 Mw 6.7 Okhotsk 10.1002/2015GL065446 deep earthquake: Additional evidence Key Points: from regional seismic stations • New regional seismic data confirm the 1,2 1 2 supershear rupture during the Mw 6.7 Zhongwen Zhan , Peter M. Shearer , and Hiroo Kanamori Okhotsk deep earthquake • The moment-rate function based on a 1Institute of Geophysics and Planetary Physics, University of California, San Diego, La Jolla, California, USA, 2Seismological joint inversion has a smooth shape without any temporal gaps Laboratory, California Institute of Technology, Pasadena, California, USA • The Mw 6.7 Okhotsk deep earthquake is more likely a continuous rupture than a triggered doublet Abstract Zhan et al. (2014a) reported supershear rupture during the Mw 6.7 aftershock of the 2013 Mw 8.3 Sea of Okhotsk deep earthquake, relying heavily on the regional station PET, which played a critical role in constraining the vertical rupture dimension and rupture speed. Here we include five more regional stations and fi ’ Correspondence to: nd that the durations of the source time functions derived from these stations are consistent with Zhan et al. s Z. Zhan, supershear rupture model. Furthermore, to reduce the nonuniqueness of deconvolution and combine the [email protected] bandwidths of different stations, we conduct a joint inversion of the six regional stations for a single broadband moment-rate function (MRF). The best fitting MRF, which explains all the regional waveforms well, has a Citation: smooth shape without any temporal gaps. The Mw 6.7 Okhotsk deep earthquake is more likely a continuous Zhan, Z., P.
    [Show full text]
  • Origin of High-Frequency Radiation During Laboratory Earthquakes
    Accepted in GEOPHYSICAL RESEARCH LETTERS Origin of high-frequency radiation during laboratory earthquakes. S. Marty1*, F. X. Passelègue2, J. Aubry1, H. S. Bhat1, A. Schubnel1 and R. Madariaga1 1Laboratoire de Géologie, École Normale Supérieure/CNRS UMR 8538, PSL Research University, 24 rue Lhomond, F-75005 Paris, France. 2École Polytechnique Fédérale de Lausanne, CH-1015 Lausanne, Switzerland. *Corresponding author: Samson Marty ([email protected]) Key points • High-frequency radiation is enhanced with both confining pressure and rupture velocity • Acoustic sensors can be used as an array to track high-frequency sources during rupture propagation • High-frequency radiation sources propagate consistently with the rupture front and are located behind it Keywords Stick-slip, high-frequency radiation, rupture velocity, back-projection, Earthquake source properties, supershear Abstract We monitor dynamic rupture propagation during laboratory stick-slip experiments performed on saw-cut Westerly granite under upper crustal conditions (10-90 MPa). Spectral analysis of high- frequency acoustic waveforms provided evidence that energy radiation is enhanced with stress conditions and rupture velocity. Using acoustic recordings bandpass filtered to 400-800 kHz (7- 14 mm wavelength) and highpass filtered above 800 kHz, we back projected high-frequency energy generated during rupture propagation. Our results show that the high-frequency radiation originates behind the rupture front during propagation and propagates at a speed close to that obtained by our rupture velocity inversion. From scaling arguments, we suggest that the origin of high-frequency radiation lies in the fast dynamic stress-drop in the breakdown zone together with Accepted in GEOPHYSICAL RESEARCH LETTERS off-fault co-seismic damage propagating behind the rupture tip.
    [Show full text]
  • Arxiv:1910.14547V3 [Physics.Geo-Ph] 27 Oct 2020
    Supershear shock front contributions to the tsunami from the 2018 Mw 7.5 Palu earthquake Faisal Amlani,1 Harsha S. Bhat,2;∗ Wim J. F. Simons,3 Alexandre Schubnel,2 Christophe Vigny2, Ares J. Rosakis4, Joni Efendi5, Ahmed Elbanna6 and Hasanuddin Z. Abidin5;7 1. Department of Aerospace and Mechanical Engineering, University of Southern California, Los Angeles, USA. 2. Laboratoire de Geologie,´ Ecole´ Normale Superieure,´ CNRS-UMR 8538, PSL Research University, Paris, France. 3. Faculty of Aerospace Engineering, Delft University of Technology, Delft, Netherlands. 4. Graduate Aerospace Laboratories, California Institute of Technology, Pasadena, California, USA. 5. BIG (Badan Informasi Geospasial / Geospatial Information Agency of Indonesia), Java, Indonesia. 6. Department of Civil and Environmental Engineering, University of Illinois at Urbana Champaign, USA. 7. Department of Geodesy and Geomatics Engineering, Institute of Technology Bandung, Indonesia. * Corresponding author: [email protected] Hazardous tsunamis are known to be generated predominantly at subduction zones by large earthquakes on dip (vertical)-slip faults. However, a moment magnitude (Mw) 7.5 earthquake on a strike (lateral)-slip fault in Sulawesi (Indonesia) in 2018 generated a tsunami that devastated the city of Palu. The mechanism by which this large tsunami originated from a strike-slip earthquake has been debated. Here we present near- field ground motion data from a GPS station that confirms that the 2018 Palu earthquake attained supershear speed, i.e., a rupture speed greater than the speed of shear waves in the host medium. We study the effect of this supershear rupture on tsunami generation by coupling the ground motion to a 1D non-linear shallow-water wave model that accounts for both the time-dependent bathymetric displacement and velocity.
    [Show full text]
  • Early and Persistent Supershear Rupture of the 2018 Magnitude 7.5 Palu Earthquake
    ARTICLES https://doi.org/10.1038/s41561-018-0297-z Early and persistent supershear rupture of the 2018 magnitude 7.5 Palu earthquake Han Bao 1, Jean-Paul Ampuero 2,3*, Lingsen Meng1, Eric J. Fielding 4, Cunren Liang3, Christopher W. D. Milliner4, Tian Feng1 and Hui Huang1 The speed at which an earthquake rupture propagates affects its energy balance and ground shaking impact. Dynamic mod- els of supershear earthquakes, which are faster than the speed of shear waves, often start at subshear speed and later run faster than Eshelby’s speed. Here we present robust evidence of an early and persistent supershear rupture at the sub-Eshelby speed of the 2018 magnitude 7.5 Palu, Indonesia, earthquake. Slowness-enhanced back-projection of teleseismic data provides a sharp image of the rupture process, along a path consistent with the surface rupture trace inferred by subpixel correlation of synthetic-aperture radar and satellite optical images. The rupture propagated at a sustained velocity of 4.1 km s–1 from its initiation to its end, despite large fault bends. The persistent supershear speed is further validated by seismological evidence of far-field Rayleigh Mach waves. The unusual features of this earthquake probe the connections between the rupture dynamics and fault structure. An early supershear transition could be promoted by fault roughness near the hypocentre. Steady rupture propagation at a speed unexpected in homogeneous media could result from the presence of a low-velocity damaged fault zone. lthough most earthquakes rupture at speeds lower than surface rupture on land where the east side moved north (positive in the shear wave velocity, faster, so-called supershear earth- Fig.
    [Show full text]
  • Gusev's Stochastic Model for the Seismic Source: High-Frequency Behavior in the Far Zone G.M
    In memoriam A.A. Gusev Gusev's stochastic model for the seismic source: high-frequency behavior in the far zone G.M. Molchan Institute of Earthquake Prediction Theory anв Mathematical Geophysics, Russian Academy of Sciences, Moscow Abstract. This paper discusses local features in the source function that generate in the far zone simultaneously (a) a quadratic decay of the source spectrum and (b) the loss of radiation directivity at high frequencies. A. Gusev drew attention to this problem and suggested that a positive solution can be obtained for earthquake rupture front with a rather complex ("lace") structure. Below we give a theoretical solution of the problem and show that the front structure can be simple enough, but not smooth. Key words. Seismic source; high frequency radiation; theoretical seismology; Fourier analysis. 1. Introduction. A. Gusev [2013, 2014, 2018] drew attention to a problem of the modeling of the seismic source. The far-zone elastic displacement for this source must have two properties: (a) 2 spectrum decaying at high frequencies (HF) and (b) the independence of HF radiation of the direction to the receiver. The first of these properties will be referred to as the omega-square behavior and the second the loss of radiation directivity. The quadratic decay of the spectrum is a common assumption in engineering practice, although it is acceptable that its frequency 1 range may be limited [Gusev et al., 2017]. A similar situation exist with respect to the universality of property (b). The corresponding counterexamples can be found in [Kurzon et al., 2014; Wen et al., 2014], related to the frequency range 0 , where 0 is the Brune [1970] corner frequency.
    [Show full text]
  • Supershear Earthquakes
    Copyright © 2020 Harsha S. Bhat SELFPUBLISHED TUFTE-LATEX.GITHUB.IO/TUFTE-LATEX Licensed under the Apache License, Version 2.0 (the “License”); you may not use this file except in compliance with the License. You may obtain a copy of the License at http://www.apache.org/licenses/LICENSE-2.0. Unless required by applicable law or agreed to in writing, software distributed under the License is distributed on an “AS IS” BASIS, WITHOUT WARRANTIES OR CONDITIONS OF ANY KIND, either express or implied. See the License for the specific language governing permissions and limitations under the License. FOREWORD This manuscript encloses all documents required to obtain a Habilitation à Diriger des Recherches from École Normale Supérieure. I have synthesised my research work on supershear earthquakes, listed below, that were con- ducted over the last 13 years in collaboration with students, postdocs and colleagues at various institutions around the world. 1. Jara, J., L. Bruhat, S. Antoine, K. Okubo, M. Y. Thomas, Y. Klinger, R. Jolivet, and H. S. Bhat (2020). “Signature of supershear transition seen in damage and aftershock pattern”. submitted to Nat. Comm. 2. Amlani, F., H. S. Bhat, W. J. F. Simons, A. Schubnel, C. Vigny, A. J. Rosakis, J. Efendi, A. Elbanna, and H. Z. Abidin (2020). “Supershear Tsunamis and insights from the Mw 7.5 Palu Earthquake”. to appear in Nat. Geosci. 3. Mello, M., H. S. Bhat, and A. J. Rosakis (2016). “Spatiotemporal properties of sub-Rayleigh and supershear rupture velocity fields : Theory and Experiments”. J. Mech. Phys. Solids. DOI: 10.1016/j. jmps.2016.02.031.
    [Show full text]
  • Tectonophysics Global Catalog of Earthquake Rupture Velocities
    Tectonophysics xxx (xxxx) xxx–xxx Contents lists available at ScienceDirect Tectonophysics journal homepage: www.elsevier.com/locate/tecto Global catalog of earthquake rupture velocities shows anticorrelation between stress drop and rupture velocity Agnès Chouneta,*, Martin Valléea, Mathieu Causseb, Françoise Courboulexc a Institut de Physique du Globe de Paris, Sorbonne Paris Cité, Université Paris Diderot, CNRS, Paris, France b Université Grenoble Alpes, IFSTTAR, CNRS, IRD, ISTerre, Grenoble 38000, France c Université Côte d’Azur, CNRS, Observatoire de la Côte d’Azur, IRD, Géoazur, Valbonne, France ARTICLE INFO ABSTRACT Keywords: Application of the SCARDEC method provides the apparent source time functions together with seismic moment, Rupture velocity depth, and focal mechanism, for most of the recent earthquakes with magnitude larger than 5.6–6. Using this Rupture propagation large dataset, we have developed a method to systematically invert for the rupture direction and average rupture Source time functions velocity V r, when unilateral rupture propagation dominates. The approach is applied to all the shallow Global earthquakes seismology (z < 120 km) earthquakes of the catalog over the 1992–2015 time period. After a careful validation process, Stress drop variability rupture properties for a catalog of 96 earthquakes are obtained. The subsequent analysis of this catalog provides Peak Ground Acceleration variability several insights about the seismic rupture process. We first report that up-dip ruptures are more abundant than down-dip ruptures for shallow subduction interface earthquakes, which can be understood as a consequence of the material contrast between the slab and the overriding crust. Rupture velocities, which are searched without any a-priori up to the maximal P wave velocity (6000–8000 m/s), are found between 1200 m/s and 4500 m/s.
    [Show full text]