logging in or signing up Ch3 Cannes Download Post to : URL : Related Presentations : Share Add to Flag Embed Email Send to Blogs and Networks Add to Channel Uploaded from authorPOINTLite Insert YouTube videos in PowerPont slides with aS Desktop Copy embed code: (To copy code, click on the text box) Embed: URL: Thumbnail: WordPress Embed Customize Embed The presentation is successfully added In Your Favorites. Views: 20 Category: Entertainment License: All Rights Reserved Like it (0) Dislike it (0) Added: October 29, 2007 This Presentation is Public Favorites: 0 Presentation Description No description available. Comments Posting comment... Premium member Presentation Transcript Ch 3: Characterization of the SFBR Earthquake Sources: Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002Overview: Overview Fault Segmentation Rupture Sources & Scenarios Geologic Slip Rates Previous Earthquakes Fault AreaArea covered by report: Area covered by reportFault Segments: Fault Segments the shortest section considered capable of repeatedly rupturing to produce large earthquakes criteria: kinematic & dynamic kinematic: geometry, structure dynamic: rupture length, displacement of previous eqs, timing, changes in slip/creep rates, microearthquakesRuptures: 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 scenariosHayward-Rogers Creek Segments: 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 reportsRupture Model Construction: Rupture Model ConstructionSan Andreas Segments: San Andreas SegmentsSlide9: ~260 ~300 ~150San Gregorio Segments: San Gregorio SegmentsCalaveras Fault Segments: Calaveras Fault SegmentsGreen Valley & Concord Faults: Green Valley & Concord FaultsGreenville Fault Segments: Greenville Fault SegmentsSegment Dimensions: Segment DimensionsFollow-up Papers: 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). You do not have the permission to view this presentation. In order to view it, please contact the author of the presentation.
Ch3 Cannes Download Post to : URL : Related Presentations : Share Add to Flag Embed Email Send to Blogs and Networks Add to Channel Uploaded from authorPOINTLite Insert YouTube videos in PowerPont slides with aS Desktop Copy embed code: (To copy code, click on the text box) Embed: URL: Thumbnail: WordPress Embed Customize Embed The presentation is successfully added In Your Favorites. Views: 20 Category: Entertainment License: All Rights Reserved Like it (0) Dislike it (0) Added: October 29, 2007 This Presentation is Public Favorites: 0 Presentation Description No description available. Comments Posting comment... Premium member Presentation Transcript Ch 3: Characterization of the SFBR Earthquake Sources: Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002Overview: Overview Fault Segmentation Rupture Sources & Scenarios Geologic Slip Rates Previous Earthquakes Fault AreaArea covered by report: Area covered by reportFault Segments: Fault Segments the shortest section considered capable of repeatedly rupturing to produce large earthquakes criteria: kinematic & dynamic kinematic: geometry, structure dynamic: rupture length, displacement of previous eqs, timing, changes in slip/creep rates, microearthquakesRuptures: 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 scenariosHayward-Rogers Creek Segments: 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 reportsRupture Model Construction: Rupture Model ConstructionSan Andreas Segments: San Andreas SegmentsSlide9: ~260 ~300 ~150San Gregorio Segments: San Gregorio SegmentsCalaveras Fault Segments: Calaveras Fault SegmentsGreen Valley & Concord Faults: Green Valley & Concord FaultsGreenville Fault Segments: Greenville Fault SegmentsSegment Dimensions: Segment DimensionsFollow-up Papers: 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).