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Date Permissions Signed
6-22-2016
Date of Award
Summer 2016
Document Type
Masters Thesis
Degree Name
Master of Science (MS)
Department
Geology
First Advisor
Caplan-Auerbach, Jacqueline
Second Advisor
Roman, Diana Christine, 1976-
Third Advisor
Housen, Bernard Arthur
Abstract
In seismology, multiplets are a series of earthquakes with similar waveforms that are thought to represent a repeating process occurring at the same location. A few studies have previously identified multiplets with waveforms that are inverted relative to one another; here termed inverted multiplets (IMs).For this study, several data sets were searched for additional examples of IMs, including earthquake swarms associated with a volcanic eruption (Mt. Spurr), a dike intrusion (Nechako Basin), dome building (Mt. St. Helens), and times of no volcanic or magmatic activity (Piton de la Fournaise [PDLF], Mt. Spurr). Source mechanisms are determined to describe what could possibly cause this phenomenon. The results suggest there are many ways to produce an IM, but that most of the viable mechanisms relate to dike intrusion. The existence of IMs in a region could be an indicator of a dike intrusion and lead to a greater understanding of subsurface processes.
Type
Text
DOI
https://doi.org/10.25710/t3kv-vr08
Publisher
Western Washington University
OCLC Number
953527894
Subject – LCSH
Dikes (Geology); Earthquake swarms; Inversion (Geophysics
Format
application/pdf
Genre/Form
masters theses
Language
English
Rights
Copying of this document in whole or in part is allowable only for scholarly purposes. It is understood, however, that any copying or publication of this thesis for commercial purposes, or for financial gain, shall not be allowed without the author's written permission.
Recommended Citation
Brann, Joel, "Mechanisms of Inverted Seismic Multiplets" (2016). WWU Graduate School Collection. 516.
https://cedar.wwu.edu/wwuet/516