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  • Elsevier  (2)
  • PANGAEA  (2)
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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Urlaub, Morelia; Petersen, Florian; Gross, Felix; Bonforte, Alessandro; Puglisi, Giuseppe; Guglielmino, Francesco; Krastel, Sebastian; Lange, Dietrich; Kopp, Heidrun (2018): Gravitational collapse of Mount Etna's southeastern flank. Science Advances, 4(10), eaat9700, https://doi.org/10.1126/sciadv.aat9700
    Publication Date: 2023-03-03
    Description: Acoustic direct line-of-sight distance measurements offshore Etna volcano by means of a network of five transponders. The data include travel times between all transponders, pressure, temperature (inside pressure tube), sound velocity, and inclination.
    Keywords: Event label; File format; File name; File size; GDS; GDS 1; GDS 2; GDS 3; GDS 4; GDS 5; Geodesy station; POS496; POS496_59-1; POS496_61-1; POS496_62-1; POS496_63-1; POS496_65-1; Poseidon; Uniform resource locator/link to raw data file
    Type: Dataset
    Format: text/tab-separated-values, 24 data points
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  • 2
    Publication Date: 2024-04-20
    Description: This dataset includes earthquake locations from a 23 months long Ocean Bottom Seismometer (OBS) experiment conducted in response to the 2014 Mw 8.1 Iquique earthquake at the northern Chilean subduction zone. The experiment is separated into two subsequent OBS networks from December 2014 until October 2016. The accompanying zip-file SEISAN_WAV.zip includes raw waveform data for all earthquakes, the file Nordic.nor (ASCII Table) that includes all phase onset picks of all earthquakes. All data in the zipped archives can be used with the SEISAN seismology software.
    Keywords: 2014 Iquique earthquake; Binary Object; Binary Object (File Size); File content; Geodetic Earthquake Observatory on the SEAfloor; GeoSEA; GEOSEA; JPIO; local earthquakes; Marcus G. Langseth; MGL1610; MGL1610_OBA3; MGL1610_OBC6; MGL1610_OBC7; MGL1610_OBC8; MGL1610_OBN1; MGL1610_OBN2; MGL1610_OBN3; MGL1610_OBN6; MGL1610_OBN7; MGL1610_OBS1; North Chile; OB01; OB010; OB012; OB013; OB014; OB015; OB02; OB03; OB05; OB06; OB07; OB09; OB10; OB12; OB13; OB14; OB15; OBA3; OBC6; OBC7; OBC8; OBN1; OBN2; OBN3; OBN6; OBN7; OBS; OBS1; Ocean bottom seismometer; OVP TORO; OVP-TORO; OVP-TORO_01; OVP-TORO_02; OVP-TORO_03; OVP-TORO_05; OVP-TORO_06; OVP-TORO_07; OVP-TORO_09; OVP-TORO_10; OVP-TORO_12; OVP-TORO_13; OVP-TORO_14; OVP-TORO_15; Pacific; SECO; SEISAN seismology software; seismicity; SO244/1; SO244/1_10-1; SO244/1_1-1; SO244/1_14-1; SO244/1_23-1; SO244/1_28-1; SO244/1_4-1; SO244/1_43-1; SO244/1_45-1; SO244/1_47-1; SO244/1_49-1; SO244/1_6-1; SO244/1_8-1; SO244/2; SO244/2_9-1_OBA3; SO244/2_9-1_OBC6; SO244/2_9-1_OBC7; SO244/2_9-1_OBC8; SO244/2_9-1_OBN1; SO244/2_9-1_OBN2; SO244/2_9-1_OBN3; SO244/2_9-1_OBN6; SO244/2_9-1_OBN7; SO244/2_9-1_OBS1; Sonne_2; South Pacific Ocean; subduction zone; The Fine Structure of a Seismogenic Zone Revealed by Aftershocks of the 2014 Iquique Mw 8.1 Earthquake
    Type: Dataset
    Format: text/tab-separated-values, 4 data points
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  • 3
    Publication Date: 2019-02-01
    Print ISSN: 0264-3707
    Electronic ISSN: 1879-1670
    Topics: Geosciences , Physics
    Published by Elsevier
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  • 4
    Publication Date: 2022-01-31
    Description: The Earth’s ocean floor deforms continuously under the influence of plate tectonic processes. In recent years, the development of deep-sea instruments using acoustic direct-path ranging allows observations of ocean floor deformation with unprecedented spatial and temporal resolution. Due to rapid technological progress, acoustic ranging emerged as a central research field to monitor seafloor deformation. Here we review recent developments and the progress of direct-path ranging applications. We discuss the methodology and examine the effects of the oceanographic environment on the measurement precision. Comparing the resolution of previous deployments, we find that the baseline uncertainty increases linearly with baseline length, at least for distances up to 3 km, but with different linear relations for each deployment. Measurements of displacement at millimeter-level precision across normal, thrust or strike-slip faults are discussed to evaluate the influence of dedicated network designs appropriate for the discrete fault geometries. Furthermore, tectonically quiet areas, such as flanks of coastal or ocean island volcanoes and passive continental margins pose substantial hazards that often lack in-situ monitoring and are therefore a significant target for the application of seafloor geodetic techniques.
    Type: Article , PeerReviewed
    Format: text
    Format: archive
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