Arctic Mid-Ocean Ridge seismicity: Results from an OBS deployment at Lokis Castle

Activity along the Arctic Mid-Ocean Ridge (AMOR) has been progressively explored over the past 20 years. Along the ridge, processes such as dike intrusion and faulting cause earthquakes. We focus on an area around the Loki’s castle hydrothermal vent field (LCVF), located on the Mohn ultra-slow sprea...

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Main Authors: Lien, Marie Eide, Pilot, Matthias, Schlindwein, Vera, Ottemöller, Lars, Barreyre, Thibaut
Format: Conference Object
Language:unknown
Published: 2022
Subjects:
Online Access:https://epic.awi.de/id/eprint/56201/
https://hdl.handle.net/10013/epic.036a590b-3548-4dec-9762-f994773fce00
id ftawi:oai:epic.awi.de:56201
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spelling ftawi:oai:epic.awi.de:56201 2023-05-15T14:27:17+02:00 Arctic Mid-Ocean Ridge seismicity: Results from an OBS deployment at Lokis Castle Lien, Marie Eide Pilot, Matthias Schlindwein, Vera Ottemöller, Lars Barreyre, Thibaut 2022 https://epic.awi.de/id/eprint/56201/ https://hdl.handle.net/10013/epic.036a590b-3548-4dec-9762-f994773fce00 unknown Lien, M. E. , Pilot, M. , Schlindwein, V. orcid:0000-0001-5570-2753 , Ottemöller, L. and Barreyre, T. (2022) Arctic Mid-Ocean Ridge seismicity: Results from an OBS deployment at Lokis Castle , EGU General Assembly 2022, Vienna, 23 May 2022 - 27 May 2022 . doi:10.5194/egusphere-egu22-7065 <https://doi.org/10.5194/egusphere-egu22-7065> , hdl:10013/epic.036a590b-3548-4dec-9762-f994773fce00 EPIC3EGU General Assembly 2022, Vienna, 2022-05-23-2022-05-27 Conference notRev 2022 ftawi https://doi.org/10.5194/egusphere-egu22-7065 2022-06-12T23:12:19Z Activity along the Arctic Mid-Ocean Ridge (AMOR) has been progressively explored over the past 20 years. Along the ridge, processes such as dike intrusion and faulting cause earthquakes. We focus on an area around the Loki’s castle hydrothermal vent field (LCVF), located on the Mohn ultra-slow spreading ridge. Ultra-slow spreading systems are strongly controlled by tectonic processes, which provide an opportunity to study almost exclusively the effect of tectonism on a hydrothermal vent field. In June 2019, we deployed a network of eight broadband ocean bottom seismometers (OBS) in an area of about 20 by 20 km around the LCVF. The OBSs were deployed for a one-year monitoring period until July 2020. We processed the OBS data using an automatic detection routine and machine learning approach to pick phases, and then located the local earthquakes based on a 1D velocity model. This provided an earthquake catalogue that was interpreted to understand the seismicity in terms of spatial and temporal distribution, and to identify fault structures. Within the broader tectonic system we aim to enhance our understanding of the LCVF. Conference Object Arctic Arctic Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Arctic
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description Activity along the Arctic Mid-Ocean Ridge (AMOR) has been progressively explored over the past 20 years. Along the ridge, processes such as dike intrusion and faulting cause earthquakes. We focus on an area around the Loki’s castle hydrothermal vent field (LCVF), located on the Mohn ultra-slow spreading ridge. Ultra-slow spreading systems are strongly controlled by tectonic processes, which provide an opportunity to study almost exclusively the effect of tectonism on a hydrothermal vent field. In June 2019, we deployed a network of eight broadband ocean bottom seismometers (OBS) in an area of about 20 by 20 km around the LCVF. The OBSs were deployed for a one-year monitoring period until July 2020. We processed the OBS data using an automatic detection routine and machine learning approach to pick phases, and then located the local earthquakes based on a 1D velocity model. This provided an earthquake catalogue that was interpreted to understand the seismicity in terms of spatial and temporal distribution, and to identify fault structures. Within the broader tectonic system we aim to enhance our understanding of the LCVF.
format Conference Object
author Lien, Marie Eide
Pilot, Matthias
Schlindwein, Vera
Ottemöller, Lars
Barreyre, Thibaut
spellingShingle Lien, Marie Eide
Pilot, Matthias
Schlindwein, Vera
Ottemöller, Lars
Barreyre, Thibaut
Arctic Mid-Ocean Ridge seismicity: Results from an OBS deployment at Lokis Castle
author_facet Lien, Marie Eide
Pilot, Matthias
Schlindwein, Vera
Ottemöller, Lars
Barreyre, Thibaut
author_sort Lien, Marie Eide
title Arctic Mid-Ocean Ridge seismicity: Results from an OBS deployment at Lokis Castle
title_short Arctic Mid-Ocean Ridge seismicity: Results from an OBS deployment at Lokis Castle
title_full Arctic Mid-Ocean Ridge seismicity: Results from an OBS deployment at Lokis Castle
title_fullStr Arctic Mid-Ocean Ridge seismicity: Results from an OBS deployment at Lokis Castle
title_full_unstemmed Arctic Mid-Ocean Ridge seismicity: Results from an OBS deployment at Lokis Castle
title_sort arctic mid-ocean ridge seismicity: results from an obs deployment at lokis castle
publishDate 2022
url https://epic.awi.de/id/eprint/56201/
https://hdl.handle.net/10013/epic.036a590b-3548-4dec-9762-f994773fce00
geographic Arctic
geographic_facet Arctic
genre Arctic
Arctic
genre_facet Arctic
Arctic
op_source EPIC3EGU General Assembly 2022, Vienna, 2022-05-23-2022-05-27
op_relation Lien, M. E. , Pilot, M. , Schlindwein, V. orcid:0000-0001-5570-2753 , Ottemöller, L. and Barreyre, T. (2022) Arctic Mid-Ocean Ridge seismicity: Results from an OBS deployment at Lokis Castle , EGU General Assembly 2022, Vienna, 23 May 2022 - 27 May 2022 . doi:10.5194/egusphere-egu22-7065 <https://doi.org/10.5194/egusphere-egu22-7065> , hdl:10013/epic.036a590b-3548-4dec-9762-f994773fce00
op_doi https://doi.org/10.5194/egusphere-egu22-7065
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