'Fault slip' presentation slideshows

1.2k views • 96 slides

Howard Zebker, Shadi Oveisgharan, Ana Bertran-Ortiz, Fayaz Onn Stanford University

UAVSAR Science Validation Experiments. Howard Zebker, Shadi Oveisgharan, Ana Bertran-Ortiz, Fayaz Onn Stanford University November 9, 2005. Summary. Purpose: design validation experiments that demonstrate the usefulness of the UAVSAR for geophysical research Approach

573 views • 57 slides

Yan Y. Kagan Dept. Earth and Space Sciences, UCLA, Los Angeles,

Yan Y. Kagan Dept. Earth and Space Sciences, UCLA, Los Angeles, CA 90095-1567, ykagan@ucla.edu , http://eq.ess.ucla.edu/~kagan.html. Tohoku earthquake: A surprise?. http://moho.ess.ucla.edu/~kagan/Seis11 .ppt. Outline of the Talk.

666 views • 52 slides

Seismic Hazard Maps

Seismic Hazard Maps. Art Frankel U.S. Geological Survey Seattle, WA. U.S. National Seismic Hazard Maps. Seismic hazard assessment integrates what we know about earthquake sources, faults, deformation, and ground motions STICK CLOSE TO THE DATA!. Geologic mapping, fault slip rates

968 views • 47 slides

A Kinematic Fault Network Model for Crustal Deformation

A Kinematic Fault Network Model for Crustal Deformation (including seismicity of optimal locking depth, shallow surface creep and geological constraints) Yuehua Zeng and Zhengkang Shen. Elastic dislocation theory. Locked near the surface. Locking Depth.

491 views • 37 slides

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453 views • 32 slides

Focal Mechanism Solutions

358 views • 28 slides

GE177b- Objectives

315 views • 24 slides

GE177b- Objectives

242 views • 24 slides

Earthquakes and crustal Deformation - Objectives of class-

245 views • 24 slides

Slip rate uncertainty: Examples from the Calico and Lenwood faults

Slip rate uncertainty: Examples from the Calico and Lenwood faults. Dr. Mike Oskin Department of Geological Sciences University of North Carolina at Chapel Hill. Co-PI : Lesley Perg Students : Mike Strane, Emily Gurney, Eitan Shelef, Dylan Blummentritt

341 views • 22 slides

Yan Y. Kagan and David D. Jackson Dept. Earth and Space Sciences, UCLA, Los Angeles,

Yan Y. Kagan and David D. Jackson Dept. Earth and Space Sciences, UCLA, Los Angeles, CA 90095-1567, ykagan@ucla.edu , http://eq.ess.ucla.edu/~kagan.html. Maximum Earthquake Size for Subduction Zones. http://moho.ess.ucla.edu/~kagan/SSA12 .ppt. Outline.

334 views • 18 slides

Inherent Mechanism Determining Scaling Properties of Fault Constitutive Laws

272 views • 16 slides

Inherent Mechanism Determining Scaling Properties of Fault Constitutive Laws

163 views • 16 slides

Ken Hudnut U.S. Geological Survey hudnut@usgs 2 2 November 2013

379 views • 14 slides

Assimilation of Continuous GPS Data into Kinematic Fault Models

127 views • 12 slides

Sedimentary Rock Formations

Sedimentary Rock Formations. Fault Slip. Folds. More Folds. Uplifted Layering. Layering. Obsidian. With Flow Banding.

202 views • 7 slides

HTDP: A tool to correct survey data for tectonic motion Chris Pearson, National Geodetic Survey

HTDP: A tool to correct survey data for tectonic motion Chris Pearson, National Geodetic Survey Richard Snay, National Geodetic Survey Rob McCaffrey, Troy Geophysics. Updated model of the secular field. An analytical model representing horizontal crustal motion developed using DEFNODE

225 views • 5 slides

Stress Accumulation at the San Andreas Fault System

Stress Accumulation at the San Andreas Fault System. Fault Slip [m]. 1857 Fort Tejon earthquake segment. Depth [km]. 1966 Parkfield earthquake segment. Central San Andreas fault creep segment. Stress [MPa]. 1906 San Francisco earthquake segment. t = 25 yr. Depth [km].

184 views • 1 slides