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        <datestamp>2021-04-02T09:36:17Z</datestamp>
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  <identifier identifierType="DOI">10.5281/ZENODO.4659820</identifier>
  <creators>
    <creator>
      <creatorName>Tolomei Cristiano</creatorName>
      <affiliation>Istituto Nazionale di Geofisica e Vulcanologia</affiliation>
    </creator>
    <creator>
      <creatorName>Polcari Marco</creatorName>
      <affiliation>Istituto Nazionale di Geofisica e Vulcanologia</affiliation>
    </creator>
    <creator>
      <creatorName>Famiglietti Nicola Angelo</creatorName>
      <affiliation>Istituto Nazionale di Geofisica e Vulcanologia</affiliation>
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  <titles>
    <title>Thessaly March 2021 coseismic  InSAR S1 displacement maps</title>
  </titles>
  <publisher>Zenodo</publisher>
  <publicationYear>2021</publicationYear>
  <subjects>
    <subject>InSAR Interferometry</subject>
    <subject>tectonic deformation</subject>
  </subjects>
  <dates>
    <date dateType="Issued">2021-04-02</date>
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    <description descriptionType="Abstract">&lt;p&gt;We study the surface deformation following a moderate size M5+ earthquake sequence which occurred close to the Tyrnavos village (Thessaly, Greece) in March 2021. We use the Interferometric Synthetic Aperture Radar (InSAR) technique exploiting several pairs of Sentinel-1 acquisitions to successfully retrieve the ground movement caused by the three major events (M5+) of the sequence. Thanks to the 6 days repeat time of the Sentinel-1 mission, InSAR analysis allowed us to detect both the surface displacement due to each of the analyzed earthquakes as well as the cumulated one occurred during the seismic sequence.&lt;/p&gt;</description>
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