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Simulation and Validation: NGA East Ralph Archuleta Department of Earth Science University of California, Santa Barbara DCPP Seismic Hazard Nov. 30, 2011 With funding from the US Nuclear Regulatory Commission (NRC), and in collaboration with the US Geological Survey (USGS) and national experts, the Pacific Earthquake Engineering Research Center has initiated a comprehensive multidisciplinary program to develop Next Generation Attenuation Relationships for the Central and Eastern North-America (NGA-East). (From PEER NGA East Website)
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Page 1: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

Simulation and Validation: NGA East

Ralph Archuleta Department of Earth Science

University of California, Santa Barbara

DCPP Seismic Hazard Nov. 30, 2011

With funding from the US Nuclear Regulatory Commission (NRC), and in collaboration with the US Geological Survey (USGS) and national experts, the Pacific Earthquake Engineering Research Center has initiated a comprehensive multidisciplinary program to develop Next Generation Attenuation Relationships for the Central and Eastern North-America (NGA-East). (From PEER NGA East Website)

Page 2: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

Finite Fault Simulation Working Group NGA East

• Pacific Engineering (W. Silva) • Regional Academy of Natural Science (A.

Bykovstev) • San Diego State/ETH (K. Olsen) • UCSB (R. Archuleta) • URS (P. Somerville) • USGS (Y. Zeng*)

DCPP Seismic Hazard Nov. 30, 2011

Page 3: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

World Stress Map Project

DCPP Seismic Hazard Nov. 30, 2011

Page 4: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

Focal Mechanisms Mostly in US

M > 3.0, 1993-2003: Saint Louis University Earthquake Center DCPP Seismic Hazard Nov. 30, 2011

Page 5: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

Focal Mechanisms in Middle America

M > 3.0, 1993-2003: Saint Louis University Earthquake Center DCPP Seismic Hazard Nov. 30, 2011

Page 6: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

Mineral Virginia Aug. 23, 2011 Mw 5.8

Afershocks from Saint Louis University Earthquake Center

DCPP Seismic Hazard Nov. 30, 2011

Page 7: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

Earthquakes for Simulations Validation There are seven earthquakes that will be used in the validation. Listed in order to perform the validation study:

2005 Riviere du Loup -- Mw 4.6 1988 Saguenay – Mw 5.8 2000 Tottori – Mw 6.7 *2011 Mineral, VA – Mw 5.8 Will be done before others. 1994 Northridge – Mw 6.7 1989 Loma Prieta – Mw 7.0 1979 Imperial Valley – Mw 6.6 1999 Chi Chi – Mw 7.6 For each earthquake the fixed parameters and the station locations are given. The validation has several elements. The first is to determine a faulting model that has minimum bias and standard deviation of the spectral acceleration response spectrum (5% damped) at periods of 10 s, 7.5 s, 5.0 s, 4.0 s, 3.0 s, 2.0 s, 1.5 s, 1.0 s, 0.5 s, 0.3 s, 0.2 s, 0.1 s and 0.05 s. The passband of the data may not allow comparisons at 10 s and 7.5 s.

DCPP Seismic Hazard Nov. 30, 2011

Page 8: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

Simulation Parameters L: Rupture length. W: Rupture width. hTop: Vertical Depth to top of rupture plane. hypoStrike: Horizontal distance along strike from top center of rupture plane to the hypocenter, in local rupture plane coordinates. hypoDip: Vertical distance along dip from top center of rupture plane to the hypocenter, in local rupture plane coordinates. hypoLat: Latitude coordinate of hypocenter. hypoLon: Longitude coordinate of hypocenter. hypoDep: Vertical depth of hypocenter. M0: Seismic moment.

DCPP Seismic Hazard Nov. 30, 2011

Page 9: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

Saguenay (Mw 5.8) Parameter Value rupL [m] 10000 ddW [m] 9900 hTop [m] 22000 hypoStrike [m] 520

hypoDip [m] 4413.5116

76 hypoLat [deg] 48.12 hypoLon [deg] -71.18 hypo [m] 26000 M0 [N-m] 5.85E+17 strike [deg] 320 dip [deg] 65 rake [deg] 78

Thickness [km] Vp [km/s] Vs [km/s] d[kg/dm^3] Qp Qs 1.44 4.5 2.6 2.3 500 250

6 5.5 3.4 2.5 1000 500 12 6.1 3.5 2.67 4000 2000 14 6.6 3.7 2.85 4000 2000 10 7 4 3.02 4000 2000 0 8.2 4.7 3.335 4000 2000

Stations

Longitude [deg]

Latitude [deg]

Vs30 (Wald & Allen, 2007) [m/s]

BSPQ -70.5057 47.4418 566.365 CHIQ -71.0123 48.4902 656.306 LMBQ -70.1527 47.6553 760 LMQ -70.3267 47.5483 467.178 QCQ -71.2760 46.7791 749.979

ROUQ -69.9966 47.4753 760 SANQ -71.9917 48.3248 760 SFA -70.8266 47.1244 500.744

SLBQ -70.0160 46.7418 760 STPQ -69.8045 47.4257 585.009 TADQ -69.7189 48.1432 760

DCPP Seismic Hazard Nov. 30, 2011

Page 10: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

Tottori (Mw 6.7) Parameter Value rupL [m] 40000 ddW [m] 20000 hTop [m] 500 hypoStrike [m] 0 hypoDip [m] 12000 hypoLat [deg] 133.35 hypoLon [deg] 35.275 hypo [m] 12500 M0 [N-m] 1.70E+19 strike [deg] 150 dip [deg] 90 rake [deg] 180

Thickness [km] Vp [km/s] Vs [km/s]

d[kg/dm^3] Qp Qs

2 5.5 3.179 2600 500 200 14 6.05 3.497 2700 500 200 12 6.6 3.815 2800 500 200 0 8.03 4.624 3100 500 200

Stations Longitude [deg] Latitude [deg] Vs30 (PEER) [m/s] OKY004 133.5018 34.9579 475.8 OKY005 133.7317 35.0098 293.4 OKY007 133.6121 34.7807 337.9 OKY008 133.9036 34.8701 450.6 OKY009 134.0923 34.9176 371.6 OKY014 133.7876 34.4462 362.2 OKY015 133.9256 35.2793 312.7 OKYH07 133.3169 35.0493 940.2 OKYH08 133.4055 34.9103 694.2 OKYH09 133.6765 35.1809 518.9 OKYH14 133.6205 34.9363 659.6 SMN002 133.0682 35.4714 138.8 SMN003 133.0929 35.1795 344 SMN004 132.9004 35.2881 281.4 SMN015 133.1704 35.3644 616.5 SMNH01 133.2604 35.2963 446.3 SMNH02 133.0856 35.2235 502.7 SMNH10 133.3031 35.5547 424.8 SMNH11 132.8033 35.4228 424.8 TTR005 133.8253 35.429 169.2 TTR006 133.6303 35.5106 352.7 TTR007 133.4902 35.2794 469.8 TTR008 133 3327 35 4227 139 2

DCPP Seismic Hazard Nov. 30, 2011

Page 11: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

Tottori (Mw 6.7)

DCPP Seismic Hazard Nov. 30, 2011

Page 12: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

Data and Synthetics

UCSB –Tottori simulation DCPP Seismic Hazard Nov. 30, 2011

Page 13: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

Bias, Confidence, Stdev

URS Simulation, Tottori DCPP Seismic Hazard Nov. 30, 2011

Page 14: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

Bias as a Function of Distance, T=1.0 s

URS Simulation, Tottori DCPP Seismic Hazard Nov. 30, 2011

Page 15: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

PGV as a Function of Distance

UCSB Simulation, Tottori DCPP Seismic Hazard Nov. 30, 2011

Page 16: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

Rivière-du-Loup (Mw 4.6)

Parameter Value hypoLat [deg] 47.75 hypoLon [deg] -69.73 hypo [m] 13000 M0 [N-m] 9.02E+15 strike [deg] 170 dip [deg] 60 rake [deg] 80

DCPP Seismic Hazard Nov. 30, 2011

Page 17: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

Saguenay (Mw 5.8)

DCPP Seismic Hazard Nov. 30, 2011

Page 18: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

Potential Simulation Earthquakes for Western US

2004 Parkfield – Mw 6.0 1999 Hector Mine – Mw 7.0 1995 Kobe – Mw 6.9 2000 Tottori – Mw 6.7 1994 Northridge – Mw 6.7 1989 Loma Prieta – Mw 7.0 1979 Imperial Valley – Mw 6.6 1999 Chi Chi – Mw 7.6 2011 Tohoku – Mw 9.1

DCPP Seismic Hazard Nov. 30, 2011

Page 19: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

Why These? 2004 Parkfield – Mw 6.0: Station density, Large variations of peak amplitudes; large accelerations for small earthquake 1999 Hector Mine – Mw 7.0: Complicated by multiple faults; geometry similar to Hosgri-Shoreline 1995 Kobe – Mw 6.9: Relevant to Hayward rupture 2011 Tohoku– Mw 9.1: Analog for Cascadia rupture 2000 Tottori – Mw 6.7: Classic strike-slip rupture, blind! 1994 Northridge – Mw 6.7: Obvious relevance, blind thrust 1989 Loma Prieta – Mw 7.0: Mixture of strike-slip and reverse 1979 Imperial Valley – Mw 6.6: Ground motion in a deep sedimentary basin. 1999 Chi Chi – Mw 7.6: Analog for Sierra Madre-Cucamonga rupture 2011 Tohoku– Mw 9.1: Analog for Cascadia rupture

DCPP Seismic Hazard Nov. 30, 2011

Page 20: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

Additional? 2004 Chuetsu – Multiple M > 6 events. Data are close to sources, hanging wall effects. 1999 Hector Mine – No good close in data. 2007 Chuetsu– Mw 6.8 (?) 2008 Iwate-Miyagi (sp?)– Mw 6.8 (?) Good hanging wall data, broke surface 2010 Darfield – Mw 7.0

DCPP Seismic Hazard Nov. 30, 2011

Page 21: Ralph Archuleta Department of Earth Science University of ......Department of Earth Science . University of California, Santa Barbara . DCPP Seismic Hazard Nov. 30, 2011 . With funding

DCPP Seismic Hazard Nov. 30, 2011


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