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        <identifier>oai:kanazawa-u.repo.nii.ac.jp:00047462</identifier>
        <datestamp>2024-06-20T06:09:24Z</datestamp>
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          <dc:title>Characteristics of non-tectonic tremors around the Lützow-Holm Bay, East Antarctica, during 2013–2015</dc:title>
          <dc:creator>平松, 良浩</dc:creator>
          <dc:creator>Tanaka, Yuya</dc:creator>
          <dc:creator>84067</dc:creator>
          <dc:creator>Hiramatsu, Yoshihiro</dc:creator>
          <dc:creator>73936</dc:creator>
          <dc:creator>80283092</dc:creator>
          <dc:creator>Ishihara, Yoshiaki</dc:creator>
          <dc:creator>16538</dc:creator>
          <dc:creator>Kanao, Masaki</dc:creator>
          <dc:creator>15168</dc:creator>
          <dc:creator>40233845</dc:creator>
          <dc:description>Characteristics of non-tectonic tremors, excited mainly by the interaction within the cryosphere, were investigated using seismic waveform data of 2013–2015 recorded at broadband stations on the east coast of the Lützow-Holm Bay (LHB), East Antarctica. The tremors were classified into three types by spectral and waveform features. Type A events have long durations, typically several hours to days, with high amplitudes of spectra over 1–8 Hz. They occur dominantly in austral summers. Type B events have characteristically irregular variations in discrete dominant frequencies in spectra. Type C events are harmonic tremors with discrete dominant frequencies in spectra that vary regularly with time. Type B and C events show similar seasonal variations: they are numerous around April and less so in austral winter. Comparison of spectra between seismic waves and infrasound, together with satellite images, suggests that type A events originated from storm-induced swells near off-LHB. Source locations of type C events and satellite images suggest that type C events are likely to result from the collision/crevassing of ice blocks in fast-sea-ice in LHB. Similar seasonal variations of type B and C events imply that these two events have similar origins.</dc:description>
          <dc:description>Embargo Period 24 months</dc:description>
          <dc:description>金沢大学理工研究域地球社会基盤学系</dc:description>
          <dc:description>journal article</dc:description>
          <dc:publisher>Elsevier</dc:publisher>
          <dc:date>2019-03-01</dc:date>
          <dc:type>AM</dc:type>
          <dc:format>application/pdf</dc:format>
          <dc:identifier>Polar Science</dc:identifier>
          <dc:identifier>77</dc:identifier>
          <dc:identifier>85</dc:identifier>
          <dc:identifier>19</dc:identifier>
          <dc:identifier>AA12240481</dc:identifier>
          <dc:identifier>1873-9652</dc:identifier>
          <dc:identifier>https://kanazawa-u.repo.nii.ac.jp/record/47462/files/SC-PR-HIRAMATSU-Y-77.pdf</dc:identifier>
          <dc:identifier>https://doi.org/10.24517/00053789</dc:identifier>
          <dc:identifier>http://hdl.handle.net/2297/00053789</dc:identifier>
          <dc:identifier>https://kanazawa-u.repo.nii.ac.jp/records/47462</dc:identifier>
          <dc:language>eng</dc:language>
          <dc:relation>10.1016/j.polar.2018.11.010</dc:relation>
          <dc:relation>http://www.elsevier.com/locate/issn/18739652</dc:relation>
          <dc:relation>http://www.elsevier.com/locate/issn/18739652</dc:relation>
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