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Massachusetts Institute of Technology

Kinematic models of interseismic deformation in Southern California

Abstract

dc:description.abstract

We develop a framework for interpreting geodetic measurements of interseismic deformation and geologic slip rate estimates in terms of block motions. This method accounts for the effects of block rotations and interseismic strain accumulation from active fults. We find that the San Andreas Fault slips close to Its Holocene rate in the Carrizo Plain (35.6 [plus-minus] 0.5 mm/yr) but is five times slower near San Bernadino (6.6 [plus-minus] 2.7 mm/yr). Thrust faults underneath Los Angeles, the Ventura Basin, and the San Gabriel range front all exhibit active shortening from 0.5 to 13.5 mm/yr. We suggest that differences between paleoseismic and block model slip rate estimates may be explained by changes in fault slip rates through the Holocene. The viscoelastic rheology of the non-brittle upper lithosphere may give rise to time dependent surface deformation though the seismic cycle. We extend a classic theory from periodic to temporally clustered earthquakes by superposing several out of phase earthquake cycles. This new model displays a much wider range of behaviors than does the periodic earthquake cycle model and provides a mechanism to explain apparent discrepancies between geologic and geodetic slip rate estimates. The potential for large earthquakes in an active fault system is determined by the balance between coseismic moment release and interseismic moment accumulation. We identify regions of local moment deficit in Southern California by comparing historical earthquake catalogs with the fault slip rate catalogs derived from both geologic and geodetic data. Large moment release deficits are localized in the northern Mojave Desert, San Jacinto fault, San Andreas fault, and the greater Los Angeles area. We estimate the

Degree

thesis:*
Department dc:contributor.department
Massachusetts Institute of Technology. Dept. of Earth, Atmospheric, and Planetary Sciences.
Grantor dc:publisher
Massachusetts Institute of Technology
Year dc:date.issued
2004

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Meade, Brendan J. (Brendan Joseph), 1975-
Advisor dc:contributor.advisor
  • Bradford H. Hager.

Subjects

dc:subject × 1

Rights

dc:rights
Statement dc:rights
  • M.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission.
Language dc:language.iso
eng

Identifiers

dc:identifier.*
Handle dc:identifier.uri
http://hdl.handle.net/1721.1/18069
OAI identifier oai:identifier
oai:dspace.mit.edu:1721.1/18069

Chain of custody

source
Harvested from
MIT
Base URL
dspace.mit.edu/oai/request
Last updated
2026-07-22
Source record
OAI-PMH GetRecord
citation

Meade, Brendan J. (Brendan Joseph), 1975-. Kinematic models of interseismic deformation in Southern California. Massachusetts Institute of Technology, 2004. http://hdl.handle.net/1721.1/18069