ch 3: characterization of the sfbr earthquake sources

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

Upload: feleti

Post on 22-Feb-2016

41 views

Category:

Documents


0 download

DESCRIPTION

Ch 3: Characterization of the SFBR Earthquake Sources. Working Group on California Earthquake Probabilities, 2002. Overview. Fault Segmentation Rupture Sources & Scenarios Geologic Slip Rates Previous Earthquakes Fault Area. Area covered by report. Fault Segments. - PowerPoint PPT Presentation

TRANSCRIPT

Page 1: Ch 3: Characterization of the SFBR Earthquake Sources

Ch 3: Characterization of the SFBR Earthquake

SourcesWorking Group on California

Earthquake Probabilities, 2002

Page 2: Ch 3: Characterization of the SFBR Earthquake Sources

OverviewFault SegmentationRupture Sources &

ScenariosGeologic Slip RatesPrevious EarthquakesFault Area

Page 3: Ch 3: Characterization of the SFBR Earthquake Sources

Area covered by report

Page 4: Ch 3: Characterization of the SFBR Earthquake Sources

Fault Segmentsthe 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

Rupturesrupture 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

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

Rupture Model Construction

Page 8: Ch 3: Characterization of the SFBR Earthquake Sources

San Andreas Segments

Page 9: Ch 3: Characterization of the SFBR Earthquake Sources

~260

~300

~150

Page 10: Ch 3: Characterization of the SFBR Earthquake Sources

San Gregorio Segments

Page 11: Ch 3: Characterization of the SFBR Earthquake Sources

Calaveras Fault Segments

Page 12: Ch 3: Characterization of the SFBR Earthquake Sources

Green Valley & Concord Faults

Page 13: Ch 3: Characterization of the SFBR Earthquake Sources

Greenville Fault Segments

Page 14: Ch 3: Characterization of the SFBR Earthquake Sources
Page 15: Ch 3: Characterization of the SFBR Earthquake Sources

Segment Dimensions

Page 16: Ch 3: Characterization of the SFBR Earthquake Sources

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).