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  • Articles  (6)
  • GFZ Data Services  (6)
  • Cham : Springer
  • RAND Corporation
  • Singapore :Springer Nature Singapore :
  • English  (6)
  • Czech
  • 2005-2009  (6)
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  • English  (6)
  • Czech
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  • 1
    Publication Date: 2020-02-12
    Description: The Iquique Local Network (ILN), a temporal network of broadband and short period seismic stations has been operating in Northern Chile since 2009. The aim of this installation was to locally densify the permanent seismic installation of the Integrated Plate Boundary Observatory in Chile (IPOC), with the main goal to decrease the magnitude of detected earthquake, to improve the hypocentral location accuracy, to allow a more accurate investigation of seismic source parameters, and to analyse proposed seismogenic structures of the Northern Chile seismic gap. The network setup evolved with time, with different geometries at different installation phases, aiming to study different seismicity features. In the first phase, started in 2009 and operational since 2010 until autumn 2013, the network had a sparse configuration, targeting a broad region extending from 19.5° S in the North to approximately 21.3° S South of Iquique. In the following stage, operational until fall 2017, most broadband stations were rearranged into a small aperture seismic array (PicArray) close to the village of Pica, to monitor with array techniques the shallow seismicity at the plate interfacer, intermediate and deep focus seismicity. These data are freely available under the Creative Commons Attribution 4.0 International Licence (CC BY 4.0) at the GEOFON data centre under network code IQ.
    Language: English
    Type: info:eu-repo/semantics/workingPaper
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  • 2
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    GFZ Data Services
    Publication Date: 2020-02-12
    Description: A temporary local seismic network was installed in the basin of Norcia (Italy) in January 2009 and operated until May 2009. Several recordings collected by the network are earthquakes of the 2009, Mw 6.3 L'Aquila seismic sequence. The seismic equipments consisted of fifteen Earth-Data Loggers (24 bit) connected to Mark L4-3D sensors (1Hz). The stations continuously recorded at a rate of 100 samples per second, and the timing was provided by a GPS link. This work was carried out in the framework of Project S4 “The Italian strong motion database”, funded within the DPC-INGV 2007–2009 Agreement, between the Italian Department of Civil Protection and the Istituto Nazionale di Geofisica e Vulcanologia. Waveform data are available from the GEOFON data centre, under network code 3H.
    Language: English
    Type: info:eu-repo/semantics/workingPaper
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  • 3
    Publication Date: 2020-02-12
    Language: English
    Type: info:eu-repo/semantics/workingPaper
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  • 4
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    GFZ Data Services
    Publication Date: 2020-11-04
    Description: After the November 14, 2007 M7.7 Tocopilla earthquake in northern Chile, a local seismic network was installed in the rupture area between approximately Tocopilla and Antofagasta by the German Task Force for earthquakes (German Research Centre for Geosciences - GFZ) in order to record aftershocks. The network was composed of 20 mostly short period seismometers (L4-3D) and 5 strong motion instruments recording continuously with a sampling rate of 100 Hz; the average distance between these stations was ~15 km. Waveform data are available from the GEOFON data centre, under network code Y9 under CC-BY 4.0 license.
    Language: English
    Type: info:eu-repo/semantics/workingPaper
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  • 5
    Publication Date: 2020-12-17
    Language: English
    Type: info:eu-repo/semantics/other
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  • 6
    Publication Date: 2021-03-24
    Description: There is a growing debate on the conventional plume model and no consensus about their deep origin. Davaille et al. (2005) showed, using fluid mechanics experiments, the existence of different class of plumes, depending on mantle thermo-chemical properties. Cape Verde is located in the interior of a slow-moving oceanic plate, away from the Mid-Atlantic Ridge, and is associated with one of the world’s largest swell. Some swells are believed to be caused by mantle plumes that rise from deep in the mantle to interact with the base of the lithosphere, while others are considered to be originated by the stress state of the lithospheric plates themselves. As part of a combined study of seismic, gravimetric, magnetic and geochemical observations in order to get a clearer picture of what is happening underneath Cape Verde we performed a first dense seismological VBB network deployment on several Cape Verde islands in 2007 and 2008. This presented a unique opportunity to assemble an important archive of high-quality seismic waveforms, recorded on oceanic volcanic islands. Waveform data are available from the GEOFON data centre, under network code 9A with CC-BY 4.0 license.
    Language: English
    Type: info:eu-repo/semantics/workingPaper
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