2026-08-04T05:20:41Zhttp://doidb.wdc-terra.org/oaip/oai

oai:doidb.wdc-terra.org:73562025-01-27T14:19:02ZDOIDBDOIDB.SEISNET

false4DOIDB.SEISNET 10.14470/4S7576570845 Eibl, Eva P.S. 0000-0002-0667-0035 Institute of Geosciences, University of Potsdam, Potsdam, 14467, Germany Hersir, Gylfi P. 0000-0002-9235-8442 GeoSurvey (ÍSOR), Reykjavik, Iceland Gudnason, Egill Á. GeoSurvey (ÍSOR), Reykjavik, Iceland Petursson, Fridgeir GeoSurvey (ÍSOR), Reykjavik, Iceland GFZ Data Services 2022 Deutsches GeoForschungsZentrum GFZ GEOFON Data Centre geofon@gfz.de Geophysical Instrument Pool Potsdam (GIPP) Institute of Geosciences, University of Potsdam, Potsdam, 14467, Germany GeoSurvey (ÍSOR), Reykjavik, Iceland Monitoring system Seismological stations In Situ/Laboratory Instruments > Magnetic/Motion Sensors > Seismometers In Situ Land-based Platforms > GEOPHYSICAL STATIONS/NETWORKS EARTH SCIENCE > SOLID EARTH > TECTONICS > VOLCANIC ACTIVITY Geophysics Passive seismic Seismometers Velocity MiniSEED Volcano Temporary 2021-01-01 2021-01-01 2022-05-03 2022-05-03 2025-01-31 en Seismic Network 10.1007/s00445-022-01622-z 10.5880/fidgeo.2022.010 https://geofon.gfz.de/waveform/archive/response/9F/2021_2022 Creative Commons Attribution 4.0 International 17GB .mseed XML "2-year seismological experiment near Fagradalsfjall, Reykjanes peninsula in 2021/22" is a two-year seismological experiment realized near the eruptive site at Fagradalsfjall on the Reykjanes peninsula, Iceland, by Eva Eibl (University of Potsdam) in collaboration with Gylfi P. Hersir, Egill Á. Gudnason and Friðgeir Pétursson from ISOR Iceland. From March to September 2021 an effusive, basaltic eruption happened in Geldingadalir near mount Fagradalsfjall on the Reykjanes peninsula. The aim of the seismic experiment was to monitor volcano-seismic signals such as LP events, VT events and tremor, before, during and after the eruption from 14 March 2021 to August 2022. We used two broadband seismometers (Nanometrics Trillium Compact 120 s) and two rotational sensors (iXblue blueSeis-3A) and stored the data on DataCubes and CommunicationCubes, respectively. Sensors were until mid-June installed on the surface and shielded from wind using a bucket. From mid-June they were buried 40cm deep in the ground at about 2 km from the eruptive vent. At any given time, at least one station recorded the seismic signals caused by the eruption. Waveform data are available from the GEOFON data centre, under network code 9F. -22.4 -22.1 63.8 63.9 Iceland Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ https://doi.org/10.13039/501100010956 GIPP201819 Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ https://doi.org/10.13039/501100010956 GIPP201921 Helmholtz Association in the frame of the Young Investigators Group VH-NG-1232 (SAIDAN)