Seismicity and Crustal Structure in North Greenland

The crustal structure of Greenland varies greatly across the island. Previous studies have revealed that the region of North Greenland differs from the rest of Greenland, with a more shallow crustal thickness. Although this region is far from any plate boundary, earthquakes do occur. Locating these...

Full description

Bibliographic Details
Main Author: Ellingsen, Annette
Format: Master Thesis
Language:English
Published: The University of Bergen 2018
Subjects:
Online Access:https://hdl.handle.net/1956/18127
id ftunivbergen:oai:bora.uib.no:1956/18127
record_format openpolar
spelling ftunivbergen:oai:bora.uib.no:1956/18127 2023-05-15T16:23:36+02:00 Seismicity and Crustal Structure in North Greenland Ellingsen, Annette 2018-06-19T22:00:12Z application/pdf https://hdl.handle.net/1956/18127 eng eng The University of Bergen https://hdl.handle.net/1956/18127 Copyright the Author. All rights reserved Greenland velocity model S-wave velocities seismikk seismiske bølger skorpestruktur https://data.ub.uio.no/realfagstermer/c000962 https://data.ub.uio.no/realfagstermer/c003287 https://data.ub.uio.no/realfagstermer/c000190 756199 Master thesis 2018 ftunivbergen 2023-03-14T17:41:53Z The crustal structure of Greenland varies greatly across the island. Previous studies have revealed that the region of North Greenland differs from the rest of Greenland, with a more shallow crustal thickness. Although this region is far from any plate boundary, earthquakes do occur. Locating these intraplate earthquakes can lead to a better understanding of the seismicity in the area. A challenge of understanding this region is the lack of seismic data available, as few seismic stations are in operation. However, four temporary stations were in operation from 2004 to 2007, and the data obtained gives new insights in the tectonic processes in the remote area. The velocity model used in this region today is a uniform velocity model for all of Greenland. Using the same velocity model for the entire island is not logical, as the crustal structure varies. It is thus beneficial to obtain a regional velocity model for North Greenland. The main objective of this thesis has been to find a new velocity model for North Greenland and this has been done using information about the crustal structure in the region. To obtain the knowledge needed, a joint inversion of receiver functions and apparent S-wave velocities has been performed. Shear wave velocity as a function of depth beneath the seismic stations was obtained and further implemented into a new regional velocity model. Earthquakes in the area were then relocated and the different locations were compared to locations obtained with the Greenland Velocity Model. Masteroppgave i geovitenskap MAMN-GEOV GEOV399 Master Thesis Greenland North Greenland University of Bergen: Bergen Open Research Archive (BORA-UiB) Greenland
institution Open Polar
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
op_collection_id ftunivbergen
language English
topic Greenland velocity model
S-wave velocities
seismikk
seismiske bølger
skorpestruktur
https://data.ub.uio.no/realfagstermer/c000962
https://data.ub.uio.no/realfagstermer/c003287
https://data.ub.uio.no/realfagstermer/c000190
756199
spellingShingle Greenland velocity model
S-wave velocities
seismikk
seismiske bølger
skorpestruktur
https://data.ub.uio.no/realfagstermer/c000962
https://data.ub.uio.no/realfagstermer/c003287
https://data.ub.uio.no/realfagstermer/c000190
756199
Ellingsen, Annette
Seismicity and Crustal Structure in North Greenland
topic_facet Greenland velocity model
S-wave velocities
seismikk
seismiske bølger
skorpestruktur
https://data.ub.uio.no/realfagstermer/c000962
https://data.ub.uio.no/realfagstermer/c003287
https://data.ub.uio.no/realfagstermer/c000190
756199
description The crustal structure of Greenland varies greatly across the island. Previous studies have revealed that the region of North Greenland differs from the rest of Greenland, with a more shallow crustal thickness. Although this region is far from any plate boundary, earthquakes do occur. Locating these intraplate earthquakes can lead to a better understanding of the seismicity in the area. A challenge of understanding this region is the lack of seismic data available, as few seismic stations are in operation. However, four temporary stations were in operation from 2004 to 2007, and the data obtained gives new insights in the tectonic processes in the remote area. The velocity model used in this region today is a uniform velocity model for all of Greenland. Using the same velocity model for the entire island is not logical, as the crustal structure varies. It is thus beneficial to obtain a regional velocity model for North Greenland. The main objective of this thesis has been to find a new velocity model for North Greenland and this has been done using information about the crustal structure in the region. To obtain the knowledge needed, a joint inversion of receiver functions and apparent S-wave velocities has been performed. Shear wave velocity as a function of depth beneath the seismic stations was obtained and further implemented into a new regional velocity model. Earthquakes in the area were then relocated and the different locations were compared to locations obtained with the Greenland Velocity Model. Masteroppgave i geovitenskap MAMN-GEOV GEOV399
format Master Thesis
author Ellingsen, Annette
author_facet Ellingsen, Annette
author_sort Ellingsen, Annette
title Seismicity and Crustal Structure in North Greenland
title_short Seismicity and Crustal Structure in North Greenland
title_full Seismicity and Crustal Structure in North Greenland
title_fullStr Seismicity and Crustal Structure in North Greenland
title_full_unstemmed Seismicity and Crustal Structure in North Greenland
title_sort seismicity and crustal structure in north greenland
publisher The University of Bergen
publishDate 2018
url https://hdl.handle.net/1956/18127
geographic Greenland
geographic_facet Greenland
genre Greenland
North Greenland
genre_facet Greenland
North Greenland
op_relation https://hdl.handle.net/1956/18127
op_rights Copyright the Author. All rights reserved
_version_ 1766011844888100864