Alexandria Digital Research Library

Investigation of the Seismic Nucleation Phase of Large Earthquakes Using Broadband Teleseismic Data

Author:
Burkhart, Eryn Therese
Degree Grantor:
University of California, Santa Barbara. Earth Science
Degree Supervisor:
Chen Ji
Place of Publication:
[Santa Barbara, Calif.]
Publisher:
University of California, Santa Barbara
Creation Date:
2014
Issued Date:
2014
Topics:
Geophysics
Keywords:
Large earthquake
Seismology
SNP
Seismic nucleation phase
Earthquake
Earthquake nucleation
Genres:
Online resources and Dissertations, Academic
Dissertation:
M.S.--University of California, Santa Barbara, 2014
Description:

The dynamic motion of an earthquake begins abruptly, but is often initiated by a short interval of weak motion called the seismic nucleation phase (SNP). Ellsworth and Beroza [1995, 1996] concluded that the SNP was detectable in near-source records of 48 earthquakes with moment magnitude (Mw), ranging from 1.1 to 8.1. They found that the SNP accounted for approximately 0.5% of the total moment and 1/6 of the duration of the earthquake. Ji et al [2010] investigated the SNP of 19 earthquakes with Mw greater than 8.0 using teleseismic broadband data. This study concluded that roughly half of the earthquakes had detectable SNPs, inconsistent with the findings of Ellsworth and Beroza [1995]. Here 69 earthquakes of Mw 7.5-8.0 from 1994 to 2011 are further examined. The SNP is clearly detectable using teleseismic data in 32 events, with 35 events showing no nucleation phase, and 2 events had insufficient data to perform stacking, consistent with the previous analysis.

Our study also reveals that the percentage of the SNP events is correlated with the focal mechanism and hypocenter depths. Strike-slip earthquakes are more likely to exhibit a clear SNP than normal or thrust earthquakes. Eleven of 14 strike-slip earthquakes (78.6%) have detectable NSPs. In contrast, only 16 of 40 (40%) thrust earthquakes have detectable SNPs. This percentage also became smaller for deep events (33% for events with hypocenter depth>250 km). To understand why certain thrust earthquakes have a visible SNP, we examined the sediment thickness, age, and angle of the subducting plate of all thrust earthquakes in the study. We found that thrust events with shallow (600 m) on the subducting plate tend to have clear SNPs. If the SNP can be better understood in the future, it may help seismologists better understand the rupture dynamics of large earthquakes.

Potential applications of this work could attempt to predict the magnitude of an earthquake seconds before it begins by measuring the SNP, vastly improving earthquake Early Warning Systems for populated areas.

Physical Description:
1 online resource (49 pages)
Format:
Text
Collection(s):
UCSB electronic theses and dissertations
ARK:
ark:/48907/f3xp7339
ISBN:
9781321567496
Catalog System Number:
990045118010203776
Rights:
Inc.icon only.dark In Copyright
Copyright Holder:
Eryn Burkhart
File Description
Access: Public access
Burkhart_ucsb_0035N_12357.pdf pdf (Portable Document Format)