Double-Difference Relocation and Empirical Green’s Function Analysis of Storfjorden Earthquakes

On 21 February 2008, an earthquake of magnitude Mw 6.1 occurred in Storfjorden on Svalbard. Since then, more than 2000 earthquakes have been recorded in this region. More recently, on 29 March 2016, an earthquake of magnitude Mw 5.2 occurred close to Edgeøya. This event marks the north-eastern exten...

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Main Author: Tjåland, Norunn
Format: Master Thesis
Language:English
Published: The University of Bergen 2017
Subjects:
Online Access:https://hdl.handle.net/1956/15947
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author Tjåland, Norunn
author_facet Tjåland, Norunn
author_sort Tjåland, Norunn
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
description On 21 February 2008, an earthquake of magnitude Mw 6.1 occurred in Storfjorden on Svalbard. Since then, more than 2000 earthquakes have been recorded in this region. More recently, on 29 March 2016, an earthquake of magnitude Mw 5.2 occurred close to Edgeøya. This event marks the north-eastern extension of the earthquake sequence. In this study, in order to improve the initial hypocenter locations, the double-difference relocation method has been applied to earthquakes in the Storfjorden area. In addition, earthquake source parameters are derived applying the empirical Green’s function method. By using smaller earthquakes in the sequence as empirical Green’s functions, the effects from path, site and instrument are removed from the seismogram of a larger correlated earthquake by deconvolution. The earthquake relocation reveals at least four NE-SW trending structures, that are steeply dipping to the south-east. Faults of other directions are also indicated from fault plane solutions. However these are not resolved in the relocation of the earthquakes. Stress drop estimates reveal a decrease of static stress drop with decreasing seismic moment. This indicates that the seismicity in Storfjorden is attributed to a complex tectonic structure that is activated under the present state of stress. Moreover, the non-constant stress drop imply varying fault properties between larger and smaller earthquakes. Masteroppgave i geovitenskap MAMN-GEOV GEOV399
format Master Thesis
genre Edgeøya
Storfjorden
Svalbard
genre_facet Edgeøya
Storfjorden
Svalbard
geographic Svalbard
Edgeøya
geographic_facet Svalbard
Edgeøya
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op_rights Copyright the Author. All rights reserved
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publisher The University of Bergen
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spelling ftunivbergen:oai:bora.uib.no:1956/15947 2025-01-16T21:41:36+00:00 Double-Difference Relocation and Empirical Green’s Function Analysis of Storfjorden Earthquakes Tjåland, Norunn 2017-06-07T22:00:07Z application/pdf https://hdl.handle.net/1956/15947 eng eng The University of Bergen https://hdl.handle.net/1956/15947 Copyright the Author. All rights reserved 756199 Master thesis 2017 ftunivbergen 2023-03-14T17:38:45Z On 21 February 2008, an earthquake of magnitude Mw 6.1 occurred in Storfjorden on Svalbard. Since then, more than 2000 earthquakes have been recorded in this region. More recently, on 29 March 2016, an earthquake of magnitude Mw 5.2 occurred close to Edgeøya. This event marks the north-eastern extension of the earthquake sequence. In this study, in order to improve the initial hypocenter locations, the double-difference relocation method has been applied to earthquakes in the Storfjorden area. In addition, earthquake source parameters are derived applying the empirical Green’s function method. By using smaller earthquakes in the sequence as empirical Green’s functions, the effects from path, site and instrument are removed from the seismogram of a larger correlated earthquake by deconvolution. The earthquake relocation reveals at least four NE-SW trending structures, that are steeply dipping to the south-east. Faults of other directions are also indicated from fault plane solutions. However these are not resolved in the relocation of the earthquakes. Stress drop estimates reveal a decrease of static stress drop with decreasing seismic moment. This indicates that the seismicity in Storfjorden is attributed to a complex tectonic structure that is activated under the present state of stress. Moreover, the non-constant stress drop imply varying fault properties between larger and smaller earthquakes. Masteroppgave i geovitenskap MAMN-GEOV GEOV399 Master Thesis Edgeøya Storfjorden Svalbard University of Bergen: Bergen Open Research Archive (BORA-UiB) Svalbard Edgeøya ENVELOPE(22.500,22.500,77.750,77.750)
spellingShingle 756199
Tjåland, Norunn
Double-Difference Relocation and Empirical Green’s Function Analysis of Storfjorden Earthquakes
title Double-Difference Relocation and Empirical Green’s Function Analysis of Storfjorden Earthquakes
title_full Double-Difference Relocation and Empirical Green’s Function Analysis of Storfjorden Earthquakes
title_fullStr Double-Difference Relocation and Empirical Green’s Function Analysis of Storfjorden Earthquakes
title_full_unstemmed Double-Difference Relocation and Empirical Green’s Function Analysis of Storfjorden Earthquakes
title_short Double-Difference Relocation and Empirical Green’s Function Analysis of Storfjorden Earthquakes
title_sort double-difference relocation and empirical green’s function analysis of storfjorden earthquakes
topic 756199
topic_facet 756199
url https://hdl.handle.net/1956/15947