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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>
          <jpcoar:creator>
            <jpcoar:creatorName>平松, 良浩</jpcoar:creatorName>
          </jpcoar:creator>
          <jpcoar:creator>
            <jpcoar:creatorName>Tanaka, Yuya</jpcoar:creatorName>
          </jpcoar:creator>
          <jpcoar:creator>
            <jpcoar:nameIdentifier nameIdentifierURI="https://kaken.nii.ac.jp/ja/search/?qm=80283092" nameIdentifierScheme="e-Rad_Researcher">80283092</jpcoar:nameIdentifier>
            <jpcoar:creatorName>Hiramatsu, Yoshihiro</jpcoar:creatorName>
          </jpcoar:creator>
          <jpcoar:creator>
            <jpcoar:creatorName>Ishihara, Yoshiaki</jpcoar:creatorName>
          </jpcoar:creator>
          <jpcoar:creator>
            <jpcoar:nameIdentifier nameIdentifierURI="https://kaken.nii.ac.jp/ja/search/?qm=40233845" nameIdentifierScheme="e-Rad_Researcher">40233845</jpcoar:nameIdentifier>
            <jpcoar:creatorName>Kanao, Masaki</jpcoar:creatorName>
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          <datacite:description descriptionType="Abstract">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.</datacite:description>
          <datacite:description descriptionType="Other">Embargo Period 24 months</datacite:description>
          <datacite:description descriptionType="Other">金沢大学理工研究域地球社会基盤学系</datacite:description>
          <dc:publisher>Elsevier</dc:publisher>
          <datacite:date dateType="Issued">2019-03-01</datacite:date>
          <datacite:date>2019-03-18</datacite:date>
          <dc:language>eng</dc:language>
          <dc:type rdf:resource="http://purl.org/coar/resource_type/c_6501">journal article</dc:type>
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          <jpcoar:identifier identifierType="DOI">https://doi.org/10.24517/00053789</jpcoar:identifier>
          <jpcoar:identifier identifierType="HDL">http://hdl.handle.net/2297/00053789</jpcoar:identifier>
          <jpcoar:identifier identifierType="URI">https://kanazawa-u.repo.nii.ac.jp/records/47462</jpcoar:identifier>
          <jpcoar:identifierRegistration identifierType="JaLC">10.24517/00053789</jpcoar:identifierRegistration>
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            <jpcoar:relatedIdentifier identifierType="DOI">10.1016/j.polar.2018.11.010</jpcoar:relatedIdentifier>
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            <jpcoar:relatedIdentifier identifierType="URI">http://www.elsevier.com/locate/issn/18739652</jpcoar:relatedIdentifier>
            <jpcoar:relatedTitle>http://www.elsevier.com/locate/issn/18739652</jpcoar:relatedTitle>
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          <jpcoar:sourceIdentifier identifierType="NCID">AA12240481</jpcoar:sourceIdentifier>
          <jpcoar:sourceIdentifier identifierType="ISSN">1873-9652</jpcoar:sourceIdentifier>
          <jpcoar:sourceTitle>Polar Science</jpcoar:sourceTitle>
          <jpcoar:sourceTitle xml:lang="en">19</jpcoar:sourceTitle>
          <jpcoar:pageStart>77</jpcoar:pageStart>
          <jpcoar:pageEnd>85</jpcoar:pageEnd>
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            <datacite:date dateType="Available">2021-04-01</datacite:date>
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