'Slip rate' presentation slideshows

ETM 5111 Introduction to Strategy, Technology and Integration

661 views • 56 slides

Eric Kirby Penn State University Collaborators:

Late Pleistocene Slip Rate Along the Owens Valley Fault. Eric Kirby Penn State University Collaborators: Sridhar Anadankrishnan, Fred Phillips, Shasta Marrero, Nancye Dawers, Doug Burbank. SCEC Fault System History January 31, 2008. Geodynamics of deformation in the ECSZ.

489 views • 35 slides

UCERF3 Statewide Fault-Model & Paleoseismic Data Workshop (SoCal)

UCERF3 Statewide Fault-Model & Paleoseismic Data Workshop (SoCal). Scott Lindvall Fugro Consultants, Inc. April 6, 2011. Recent Modifications to UCERF2 Fault Sources for Seismic Hazard Evaluation of LADWP Van Norman Complex San Fernando Valley and Transverse Ranges.

411 views • 30 slides

Kern County Earthquake

Kern County Earthquake. Vertical fracture on the northeast side of Bear Mountain, along the White Wolf Fault. At this location, a vertical displacement of 60 cm (2 ft) and a horizontal (left-lateral) displacement of 45 cm (1.5 ft) were measured along the break. Vital stats.

536 views • 26 slides

Exploring uncertainties in millennial slip rates along the eastern Kunlun fault, NE Tibet

Exploring uncertainties in millennial slip rates along the eastern Kunlun fault, NE Tibet. Nathan Harkins PSU Geosciences. Eric Kirby and Xuhua Shi. SCEC Joint Fault System History / SoSAFE Workshop 1/31/2008. Motivation: Terrace risers as slip markers.

382 views • 26 slides

A New Approach To Paleoseismic Event Correlation

397 views • 26 slides

What geologic input do we need? Representation of the fault. Slip rate on the fault.

What geologic input do we need? Representation of the fault. Slip rate on the fault. The frequency of ground rupturing events at a point. The extent of the ground ruptures (i.e. size of event). The frequency of ground rupturing events at a point. Can be determined by:

347 views • 24 slides

Deterministic Seismic Hazard Analysis

Deterministic Seismic Hazard Analysis. Earliest approach taken to seismic hazard analysis Originated in nuclear power industry applications Still used for some significant structures Nuclear power plants Large dams Large bridges Hazardous waste containment facilities

751 views • 24 slides

SLICING UP THE BAY AREA: Insights from regional block modeling of GPS

347 views • 23 slides

Aftershocks follow the Omori Law (seismicity rate decays as 1/t)

Aftershocks tend to fall preferentially in area of static Coulomb stress increase but there are also earthquakes in area of decrease Coulomb stress. Aftershocks follow the Omori Law (seismicity rate decays as 1/t).

434 views • 21 slides

Active Folding within the L.A. Basin with a focus on:

Aron Meltzner. Ge 277. 21 November 2008. Active Folding within the L.A. Basin with a focus on: Argus et al. (2005), Interseismic strain accumulation and anthropogenic motion in metropolitan Los Angeles and

446 views • 19 slides

Southern San Andreas Fault

Southern San Andreas Fault. Quiescence period: 300+ years Slip rate: from 10 to 35 mm/yr Observed creep episodes. How pervasive is creep on the southern SAF? What fraction of the elastic strain energy does it relieve?

303 views • 13 slides

Captain Spratt, 1851 (Travels and researches in Crete):

Captain Spratt, 1851 (Travels and researches in Crete):

213 views • 12 slides

UCERF2 Deformation Model Can we do better in UCERF3?

215 views • 11 slides

Comments on physical simulator models

Comments on physical simulator models. David D. Jackson, UCLA. Forecast capabilities. Statistical distributions of earthquakes on prespecified faults Magnitude frequency Temporal (recurrence) for initiation, participation, and combinations Spatial

212 views • 10 slides

LiDAR and the San Andreas Fault exercise

LiDAR and the San Andreas Fault exercise. Sarah Robinson ASU. Plate tectonics and earthquakes. Wallace Creek Field Trip. Download kmz here: http://cordillera.la.asu.edu/field_trip/WallaceCreekFieldTrip5.kmz.

387 views • 7 slides

Geodetic Constraints on W and R

Geodetic Constraints on W and R. Jessica Murray Nov. 1, 2006. Resolution of Coseismic Slip. From inversion of Parkfield area geodetic data (GPS, EDM). Resolution 5 km below Carr Hill. Resolution 5 km below a point 3 km SE of Gold Hill. Langbein et al., BSSA , 2006.

193 views • 6 slides

Recurrence Intervals

325 views • 4 slides

Data Uncertainties :

313 views • 3 slides

170 views • 1 slides