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Meeting Abstracts

The SCEC collaboration emphasizes the connections between information gathering by sensor networks, fieldwork, and laboratory experiments; knowledge formulation through physics-based, system-level modeling; improved understanding of seismic hazard; and actions to reduce earthquake risk and promote resilience. Use the form below to search and view all poster and invited talk abstracts submitted to this meeting.


  
  

A SCEC username is required to submit an abstract.

The person submitting the abstract is automatically the First Author, and will receive all communications regarding the abstract.

First Authors can submit a maximum of one poster presentation abstract and one oral presentation abstract (if invited as a plenary speaker).

Abstracts should not exceed 2,500 characters in length.

Every poster will be on display from Sunday evening through Tuesday evening.

Poster dimensions cannot exceed 45 inches high x 45 inches wide.

You may upload a PDF of your poster at any time, even after the submission deadline.

Results 151-200 of 305
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SCEC ID Category Title and Authors SCEC Award
Poster
096
Geodesy Seismogenic structure and coseismic slip distribution of the 2013 Ms7.0 Lushan earthquake in southwestern China
Qi Liu, Xueze Wen, Zhigang Shao
To further understand the tectonic process of the Lushan MS7.0 earthquake, which occurred in southwestern China on April 20, 2013, a 3D fault geometry model was built by integrating the relocated aftershocks distribution and the information of... more

Poster
035
Seismology Separating non-diffuse component from ambient seismic noise cross-correlation in southern California
Xin Liu, Gregory Beroza, Nori Nakata
Cross-correlation of fully diffuse wavefields provides Green’s function between receivers, although the ambient noise field in the real world contains both diffuse and non-diffuse fields. The non-diffuse field potentially degrades the correlation... more

Poster
104
Geodesy Integration of InSAR and GPS data for 3-dimensional crustal deformation mapping
Zhen Liu, Zheng-Kang Shen, Cunren Liang, Paul Lundgren
GPS and InSAR are complementary to each other for crustal deformation mapping, with the former offering discrete high-fidelity 3-dimensional (3-D) point positioning while the latter providing 2-D dense spatial coverage of deformation measured along... more

Poster
004
EFP Space-time earthquake rate models for one-year hazard forecasts in Oklahoma
Andrea Llenos, Andrew Michael
The recent one-year seismic hazard assessments for natural and induced seismicity in the central and eastern US (CEUS) (Petersen et al., 2016, 2017) rely on earthquake rate models based on declustered catalogs (i.e., catalogs with foreshocks and... more

Poster
311
CEO 2017 UseIT: Probability Team
Chi Loh, Olivia Dorencz, Aide Escanuela, Kevin Qualls, Kevin Milner, Thomas Jordan, Jozi Pearson, Gabriela Noriega
California is a high seismic-hazard area due to several dangerous faults that run through the state, primarily the San Andreas Fault (SAF). The dense population near the SAF in cities such as Los Angeles and San Francisco makes this hazard a... more

Poster
107
Geodesy InSAR coherence time series - soil moisture as a proxy for alluvial fan age?
Rowena Lohman, Chelsea Scott, Teresa Jordan
When scientists can determine the ages of surfaces within a tectonically active area, they can turn observations of offsets and deformation into rates, repeat times and evaluations of hazard. Here, we explore the use of InSAR coherence time series... more

Poster 257
GM Ground-Motion Variance from Modeling of Multiple Rupture-Directivity Scenarios on the Newport-Inglewood/Rose Canyon Fault System
John Louie, Mounira Boudjema, Michelle Dunn, Graham Kent
We use LLNL’s SW4 wave-propagation modeler to produce shaking maps and synthetic seismograms for hypothetical, nonetheless geologically plausible earthquake ruptures of the Newport Inglewood Rose Canyon (NI/RC) fault system along the Southern... more

Poster
158
SAFS Rupture propagation through the Big Bend of the San Andreas Fault: a dynamic modeling case study of the Great Earthquake of 1857
Julian Lozos
The great San Andreas Fault (SAF) earthquake of 9 January 1857, estimated at M7.9, was one of California’s largest historic earthquakes. Its ~360 km rupture trace follows the Carrizo and Mojave segments of the SAF, including the ~30° compressional... more

Talk Tue 10:40
SAFS Introducing the Cajon Pass Earthquake Gate Area
Julian Lozos, Craig Nicholson, Nate Onderdonk
Cajon Pass is the primary junction between the San Andreas (SAF) and San Jacinto (SJF) faults. Its location in western San Bernardino County – in the middle of the densely populated Inland Empire – means that even a local rupture within the Pass... more

Poster
002
EFP Natural Time and Nowcasting Induced Seismicity at the Groningen Gas Field in the Netherlands
Molly Luginbuhl, Donald Turcotte, John Rundle
The area surrounding the Groningen natural gas field in the Netherlands has recently seen a significant increase in seismicity. How to handle this induced seismicity has become a controversial topic for many. The gas field provides energy for the... more

Poster
184
FARM Dynamics of Non-planar Thrust Faults Governed by Various Friction Laws
Bin Luo, Benchun Duan
Fault interface topography is a prevailing factor in earthquake rupture dynamics. In subduction zones, large-scale oceanic reliefs such as seamounts and plateaus on the incoming oceanic plate can be subducted with the downgoing plate, giving rise to... more

Poster
208
SDOT Borehole Breakouts Versus Earthquake Focal Mechanisms as Stress Field Orientation Indicators in Southern California: Should We Agree to Disagree?
Karen Luttrell, Jeanne Hardebeck
One of the SCEC5 priorities is the development of an internally consistent group of Community Models (CXM), including the maturation of the Community Stress Model (CSM). Many of the geodynamic models that integrate multiple physical processes into... more
17174
Poster
260
GM Taiwan Earthquake Model: PSHA and Scenario Hazard Map
Kuo-Fong Ma, Taiwan Earthquake Model (TEM) team
Taiwan Earthquake Model (TEM) using GEM OpenQuake engine for the assessment of seismic hazards of Taiwan. The first version of TEM probabilistic seismic hazard analysis for Taiwan was published in 2015 (TEM PSHA2015, Wang et al., 2016a). The model... more

Poster
180
FARM Stick Slip Instabilities and Strain Localization Dynamics in a fluid-infiltrated fault gouge zone model
Xiao Ma, Ahmed Elbanna
Stick-slip instabilities and shear localization have been long observed in sheared fault gouge, yet their underlying microscopic mechanisms are still not fully understood. Although numerous studies of the stick slip behavior within fault gouge have... more

Poster
302
CME Current Capabilities of the SCEC Unified Community Velocity Model (UCVM) Software Framework
Philip Maechling, Ricardo Taborda, Kim Olsen, Scott Callaghan, Thomas Jordan, Christine Goulet
The Southern California Earthquake Center (SCEC) has developed the Unified Community Velocity Model (UCVM) software framework to facilitate the registration and distribution of existing and future seismic velocity models to the SCEC community. The... more

Poster
268
GM Cluster analysis of the long-period ground-motion simulation data – application of the Nankai Trough megathrust earthquakes scenarios
Takahiro Maeda, Hiroyuki Fujiwara, Toshihiko Hayakawa, Satsuki Shimono, Sho Akagi
Extracting important hazard information and its trends from the big data leads to better risk assessment and quick respond in case of emergency when megathrust earthquake happens. A cluster analysis was applied to the big data of the long-period... more

Talk
Mon 14:00
EFP Progresses and challenges for Operational Earthquake Forecasting in Italy
Warner Marzocchi
Tracking the time evolution of seismic hazard in time windows shorter than the usual 50-years of long-term hazard models may offer additional opportunities to reduce the seismic risk. This is the target of operational earthquake forecasting (OEF) as... more

Poster
216
SDOT Measuring Aseismic Slip through Characteristically Repeating Earthquakes at the Mendocino Triple Junction
Kathryn Materna, Taka'aki Taira, Roland Bürgmann
The Mendocino Triple Junction (MTJ) is located at the seismically active transition between the San Andreas fault system, the Mendocino Transform Fault, and the Cascadia Subduction Zone. Most of the major faults of the triple junction are located... more

Talk
Wed 11:00
EEII Post-Earthquake Reconnaissance: a Structural Engineer’s Perspective
Silvia Mazzoni
Post-Earthquake Reconnaissance gives a first-hand opportunity to observe the effects of an earthquake on a human scale. During a reconnaissance, we gather data and knowledge, as well as an understanding and appreciation of the interdependencies... more

Poster
109
Geology Examining earthquake processes with microtextural analysis and (U-Th)/He thermochronometry: a case study from hematite fault mirrors in the Wasatch fault zone
Robert McDermott, Alexis Ault, James Evans
Advances in physically based models of earthquake rupture place an increasing importance on characterization of the physical processes that control dynamic friction in natural faults. We apply coupled textural analysis and hematite (U-Th)/He (He)... more

Poster
161
SAFS Puzzling results in a slip rate study for the Banning Strand of the San Andreas Fault near North Palm Springs
Sally McGill, Paula Figueiredo, Lewis Owen
To better understand the likely rupture paths and slip distribution on the southern San Andreas Fault, additional slip rate measurements are needed from the Mission Creek, Banning and Garnet Hill fault strands in northern Coachella Valley. We... more
15182
Poster
052
Seismology Directly Estimating Rupture Area to Remove the Uncertainty in Stress Drop
Jeff McGuire, Yoshihiro Kaneko
The key kinematic earthquake source parameters: rupture velocity, duration and area, shed light on earthquake dynamics. They can provide direct constraints on stress drop and have implications for seismic hazard. However, for moderate and small... more
16104
Poster
160
SAFS Assessing stratigraphic correlations and fault zone extent at the 18th Ave trench site, Banning strand of the San Andreas Fault, North Palm Springs, California
James McNeil, Doug Yule, Katherine Scharer, Sally McGill, Devin McPhillips, Bryan Castillo, Alan Pace
A trench opened in March, 2017 by Petra Geoscience, Inc., provided a valuable opportunity to examine the previously unconstrained earthquake record of Banning strand of the San Andreas Fault (also see Castillo et al., this meeting). The initial... more
15182
Poster
122
Geology Sources and Magnitudes of Uncertainty in Fault Slip Rate, Cucamonga Thrust Fault, Southern California
Devin McPhillips, Katherine Scharer
Maps of historic earthquake ground surface ruptures show that displacements along strike are spatially variable. As a result, latest Quaternary slip rates developed from a small number of displacement measurements may not accurately represent fault... more

Poster
063
Seismology What does an 'average' large subduction earthquake look like?
Men-Andrin Meier, Jean-Paul Ampuero, Thomas Heaton
When we study individual earthquakes we often notice and report 'peculiarities', or unexpected rupture behavior. This implies that there is a 'normal' or average earthquake behavior from which such events deviate. From an... more

Poster
060
Seismology Reconciling Fault Geometry in Nepal Himalaya using the “NAMASTE” Seismic Network
Manuel Mendoza, Abhijit Ghosh, Marianne Karplus, John Nabelek, Soma Sapkota, Lok Adhikari, Simon Klemperer, Aaron Velasco
The Mw 7.8 Gorkha earthquake in April of 2015 produced ~8 m of peak co-seismic slip as the Main Himalayan Thrust (MHT) fault ruptured 130 km east, under dense population centers such as Kathmandu. The mainshock and subsequent aftershocks killed over... more

Poster
053
Seismology Towards quasi-automated estimates of directivity and related source properties of small to moderate earthquakes with second seismic moments
Haoran Meng, Yehuda Ben-Zion, Jeff McGuire
We develop a method for quasi-automated estimation of directivity, rupture area, duration, and centroid velocity of earthquakes with second seismic moments. The method is applied to small to moderate earthquakes in southern California. P and S phase... more
17177
Poster
256
GM Improving Distance Metrics in Ground Motion Prediction Equations Based with Seismic Array Back-Projections
Lingsen Meng, Tian Feng
Traditional Ground Motion Prediction Equations (GMPEs) measure the distances either relative to the epicenter (Repi) or the hypocenter (Rhyp) assuming point-sources, or relative to the closest point of the fault rupture (Rrup) or its surface... more

Poster
183
FARM Pulse-Like Partial Ruptures and High-Frequency Radiation at Creeping-Locked Transition during Megathrust Earthquakes
Sylvain Michel, Jean-Philippe Avouac, Nadia Lapusta, Junle Jiang
Megathrust earthquakes tend to be confined to fault areas locked in the interseismic period and often rupture them only partially. For example, during the 2015 M7.8 Gorkha earthquake, Nepal, a slip pulse propagating along strike unzipped the bottom... more

Poster
100
Geodesy Capturing Postseismic Processes of the 2016 Mw 7.1 Kumamoto Earthquake, Japan, Using Dense, Continuous GPS and Short-repeat Time ALOS-2 InSAR Data: Implications for the Shallow Slip Deficit Problem
Chris Milliner, Roland Bürgmann, Teng Wang, Asaf Inbal, David Bekaert, Cunren Liang, Eric Fielding
Separating the contribution of shallow coseismic slip from rapidly decaying, postseismic afterslip in surface rupturing events has been difficult to resolve due to the typically sparse configuration of GPS networks and long-repeat time of InSAR... more

Poster
012
EFP Are Physics-Based Simulators Ready for Prime Time? Comparisons of RSQSim with UCERF3 and Observations
Kevin Milner, Bruce Shaw, Jacquelyn Gilchrist, Thomas Jordan
Probabilistic seismic hazard analysis (PSHA) is typically performed by combining an earthquake rupture forecast (ERF) with a set of empirical ground motion prediction equations (GMPEs). ERFs have typically relied on observed fault slip rates and... more
16273
Talk
Wed 08:30
Seismology The Limits of Earthquake Early Warning
Sarah Minson, Annemarie Baltay, Elizabeth Cochran, Thomas Hanks, Men-Andrin Meier
The objective of earthquake early warning (EEW) is to provide population centers with a useful warning of impending strong ground shaking: the warning must be sufficiently rapid and accurate for users to take action to mitigate damage. By... more

Poster
197
FARM Grain boundary sliding triggers coeval pseudotachylyte development in brittle-ductile transition mylonites: an Electron Backscatter Diffraction (EBSD) case study of mid-crustal interseismic and coseismic deformation
Elena Miranda, Craig Stewart, Kelly Lourcey
Exposures of coeval pseudotachylytes and mylonites are relatively rare, but are crucial for understanding the seismic cycle in the vicinity of the brittle-ductile transition (BDT). We use both field observations and electron backscatter diffraction... more
17063
Poster
148
Geology Lidar data, geologic mapping, and paleoseismic trenching reveal late Quaternary surface ruptures and increased seismic hazard in southwestern British Columbia, Canada
Kristin Morell, Christine Regalla, Colin Amos, Scott Bennett, Audrey Graham, Lucinda Leonard, Emerson Lynch, Nicolas Harrichhausen
Lidar topography, structural-geomorphic mapping, and paleoseismic trenching reveal new evidence for late Quaternary activity on three faults on Vancouver Island, British Columbia, that were previously thought to be inactive since the Eocene. Two... more

Poster 236
EEII Using Spatial Variation of kappa to Develop Site-Specific Attenuation Model for Improved Broadband Simulations
Ramin Motamed, Swasti Saxena, John Anderson
Reliable synthetics are an alternative for use in engineering practice for dynamic time history analysis of geotechnical and structural systems, and this study aims to improve upon Broadband simulations to account for site-specific surface response... more
16165
Poster
003
EFP Towards Testing Probabilistic Seismic Hazard Estimates
Mostafa Mousavi, Gregory Beroza
Hazard curves in PSHA models are used for quantifying the seismic hazards by providing the annual rates of exceedance, the reciprocal of the return period, at various ground-motion levels. Beginning in 2016, the U.S. Geological Survey (USGS) started... more

Poster
276
CS Manage I/O Task in a Normalized Cross-Correlation Earthquake Detection Code for Large Seismic Datasets
Dawei Mu, Pietro Cicotti, Yifeng Cui
We have developed a high-performance GPU-based software called “cuda Normalized Cross-Correlation” (cuNCC), for calculating seismic waveform similarity for subjects like hypocenter estimates and small earthquake detection. We present the performance... more

Poster
222
SDOT Revised (lower) slip rate for the Northern Death Valley Fault based on a new method for restoring alluvial fan cutoff lines
Karl Mueller, Ragan Anthony
Determining slip rates on active strike slip faults in Southern California at timescales of 103 – 105 years depends on recognition and measurement of offset landforms and deposits. While offset deposits can be directly age dated to determine slip... more

Poster
090
Geodesy The impact of model prediction error in designing geodetic networks for crustal deformation applications
Jessica Murray
Earth surface displacements measured at Global Navigation Satellite System (GNSS) sites record crustal deformation due, for example, to slip on faults underground. A primary objective in designing geodetic networks to study crustal deformation is... more

Poster
210
SDOT InSAR and GPS time series analysis in areas with large scale hydrological deformation: separating signal from noise at varying length scales in the San Joaquin Valley
Kyle Murray, Rowena Lohman
Areas of large-scale subsidence are observed over much of the San Joaquin Valley of California due to the extraction of groundwater and hydrocarbons from the subsurface.These signals span regions with spatial extents of up to 100 km and have rates... more

Poster
022
SP Towards a High-Resolution Velocity Model with a Very Dense Array at Diablo Canyon, California
Nori Nakata, Gregory Beroza
Correlation-based analyses of ambient seismic wavefields is a powerful tool for retrieving subsurface information such as stiffness, anisotropy, and heterogeneity at a variety of scales. Especially with very dense arrays recently used for... more

Poster
234
CXM Community Fault Model Version 5.2: Updating & expanding the CFM 3D fault set and its associated fault database
Craig Nicholson, Andreas Plesch, John Shaw
We present an updated version of the SCEC Community Fault Model (CFM) for southern California. For version 5.2, we continue to focus on expanding and improving the database component of CFM that is critical for the internal consistency and... more
17027, 17066
Poster
249
GM Fourth-Order Staggered-Grid Finite-Difference Seismic Wavefield Estimation Using a Discontinuous Mesh Interface (WEDMI)
Shiying Nie, Daniel Roten, Kim Olsen, Steven Day
In a realistic geological structure with a large contrast in seismic wave speed between shallow and deep regions, simulation of seismic wave propagation using a spatially uniform grid can be computationally very demanding, due to overdiscretization... more

Poster
083
Seismology How NSHMP 2014 and UCERF3 have changed the earthquake risk landscape in the US
Marleen Nyst, Delphine Fitzenz, Nilesh Shome
Early 2017 RMS released an updated North America Earthquake Model to the insurance market with risk models for the US, Canada and Mexico. Here we will focus on California, the Pacific Northwest (PNW) and New Madrid. This new model has updates for... more

Poster 006
EFP On secular spatial seismicity
Yosihiko Ogata
It has been passed 15 years since the hierarchical (i.e., location-dependent) space-time ETAS (HIST-ETAS) models have been proposed (Ogata et al., 2003); and the short-term (daily) and intermediate-term (3-months and one year) earthquake forecasts... more

Poster
124
Geology Strath terraces in the Santa Ynez Valley suggest late Quaternary activity on a detachment fault beneath the Western Transverse Ranges, California
Nate Onderdonk, Andrew Farris, Edward Tyler, Ani Pytlewski, Antonio Garcia, Shannon Mahan
High rates of shortening across the western Transverse Ranges (WTR) have been interpreted from geodetic, geologic, and geomorphic data. Studies of active deformation of the WTR have been focused on structures along the Ventura-Santa Barbara coast.... more

Poster
114
Geology The rock record of seimic nucleation: a case study from the Whipple Mountains Detachment Fault, eastern California
Daniel Ortega-Arroyo, Whitney Behr, Emilie Gentry
Despite advances in our understanding of the physics of earthquakes, the mechanisms by which dynamic rupture nucleates in the middle crust remains enigmatic. Proposed mechanisms include flash heating of asperities, thermal pressurization of pore... more

Poster
232
CXM Toward a Geologic Framework for the Community Rheology Model, with focus on the Mojave region
Michael Oskin, Whitney Behr, Alex Morelan, Andreas Plesch, John Shaw
Strain accrues heterogeneously across southern California due to the interaction of plate-boundary driving forces with lithospheric structure. To understand this process, we undertake the construction of a geologic framework for the Community... more

Poster
017
EFP Characterizing the Triggering Susceptibility of Characteristic Faults
Morgan Page, Nicholas van der Elst, Bruce Shaw
Statistical averages of earthquake triggering behavior, namely Gutenberg-Richter magnitude scaling, can produce foreshock probabilities that differ by orders of magnitude from fault-specific methods that employ characteristic magnitude distributions... more

Poster 147
Geology Paleoseismic Record of Three Holocene Earthquakes Rupturing the Issyk-Ata Fault near Bishkek, North Kyrgyzstan
Magda Patyniak, Angela Landgraf, Atyrgul Dzhumabaeva, Kanatbek Abdrakhmatov, Swenja Rosenwinkel, Oliver Korup, Frank Preusser, Jens Fohlmeister, Ramon Arrowsmith, Manfred Strecker
The evaluation of thrust paleoearthquakes and associated fault scarps is often hampered by the size of their cumulative fault scarps and interaction with sedimentary processes during interseismic periods. This is especially true if these events... more


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