ch 3: characterization of the sfbr earthquake sources working group on california earthquake...

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Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002

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Page 1: Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002

Ch 3: Characterization of the SFBR Earthquake

SourcesWorking Group on California

Earthquake Probabilities, 2002

Page 2: Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002

Overview

Fault SegmentationRupture Sources &

ScenariosGeologic Slip RatesPrevious EarthquakesFault Area

Page 3: Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002

Area covered by report

Page 4: Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002

Fault Segments

the shortest section considered capable of repeatedly rupturing to produce large earthquakes

criteria: kinematic & dynamickinematic: geometry, structuredynamic: rupture length, displacement

of previous eqs, timing, changes in slip/creep rates, microearthquakes

Page 5: Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002

Ruptures

rupture source: single or combination of adjacent fault segments; floating eq

rupture scenario: combination of rupture sources that describe mode of failure of the entire fault during one eq cycle

rupture model: weighted combinations of the fault-rupture scenarios

Page 6: Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002

Hayward-Rogers Creek Segments

140 km long 3 segments: 9±2

RC: 8.4±2, 235-387 HN: 10±1, 270-710 HS: 7-10, 150-250 N,

130±40 S Tule Pond creep 4-6

change in timing constraint from previous reports

Page 7: Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002

Rupture Model Construction

Page 8: Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002

San Andreas Segments

Page 9: Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002

~260

~300

~150

Page 10: Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002

San Gregorio Segments

Page 11: Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002

Calaveras Fault Segments

Page 12: Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002

Green Valley & Concord Faults

Page 13: Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002

Greenville Fault Segments

Page 14: Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002
Page 15: Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002

Segment Dimensions

Page 16: Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002

Follow-up Papers Segall, P., and Lisowski, M., 1990, Surface displacements in the 1906 San

Francisco and 1989 Loma Prieta earthquakes: Science, v. 250, no. 4985, p. 1241-1244.

Schwartz, D.P., Pantosti, D., Okumura, K., Powers, T., and Hamilton, J., 1998, Paleoseismic investigations in the Santa Cruz Mountains: Implications for the recurrence of large magnitude earthquakes on the San Andreas Fault: Journal of Geophysical Research, v. 103, p. 17,985-18,001.

Thatcher, W., Marshall, G., and Lisowski, M., 1997, Resolution of fault slip along the 470-km- long rupture of the great 1906 San Francisco earthquake: Journal of Geophysical Research, v. 102, no. B3, p. 5353-5367.

Lettis, W., 2001, Late Holocene behavior and seismogenic potential of the Hayward-Rodgers- Creek fault system in the San Francisco Bay area, California: Calif. Geol. Surv. Bulletin, v. 210, p. 167-178.

C. Goldfinger et al., Rupture lengths and temporal history of significant earthquakes on the offshore and north coast segments of the Northern San Andreas Fault based on turbidite stratigraphy, Earth Planet. Sci. Lett. (2006).