<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
 <record>
  <leader>     caa a22        4500</leader>
  <controlfield tag="001">445846798</controlfield>
  <controlfield tag="003">CHVBK</controlfield>
  <controlfield tag="005">20180317145401.0</controlfield>
  <controlfield tag="007">cr unu---uuuuu</controlfield>
  <controlfield tag="008">170323e20111201xx      s     000 0 eng  </controlfield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">10.1007/s10518-011-9273-3</subfield>
   <subfield code="2">doi</subfield>
  </datafield>
  <datafield tag="035" ind1=" " ind2=" ">
   <subfield code="a">(NATIONALLICENCE)springer-10.1007/s10518-011-9273-3</subfield>
  </datafield>
  <datafield tag="245" ind1="0" ind2="0">
   <subfield code="a">Site effects observed in alluvial basins: the case of Norcia (Central Italy)</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[D. Bindi, L. Luzi, S. Parolai, D. Di Giacomo, G. Monachesi]</subfield>
  </datafield>
  <datafield tag="520" ind1="3" ind2=" ">
   <subfield code="a">In this work, we investigate the site amplification effects observed in the Norcia plain, Central Italy. Data from 30 selected local earthquakes (2 ≤ Ml ≤ 4.1) recorded by a temporary seismic network composed by 15 stations, are analyzed to determine the spatial variability of site effects. Both the Horizontal-to-Vertical spectral ratio and the Standard Spectral Ratio techniques are applied to estimate the site amplification effects. The results show that most of the sites in the valley are affected by strong amplifications (up to a factor of 20) in the frequency range 0.5-5Hz. The value of the fundamental frequency of resonance is strictly dependent on the location within the basin and on the sediment thickness. Strong amplifications also affect the vertical components. The time-frequency analysis performed on a station located inside the basin shows the presence of a large spectral amplitudes after the S-wave phase, not observed on a station located on the bedrock, suggesting the presence of locally generated wave trains. Then, in agreement with earlier observations for other alluvial basins in Central Italy, 2D-3D effects play an important role in determining the site amplification effects in Norcia.</subfield>
  </datafield>
  <datafield tag="540" ind1=" " ind2=" ">
   <subfield code="a">Springer Science+Business Media B.V., 2011</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Site effects</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Alluvial basin</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Horizontal-to-vertical spectral ratio</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Standard spectral ratio</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Bindi</subfield>
   <subfield code="D">D.</subfield>
   <subfield code="u">GFZ German Research Centre for Geosciences, Centre for Disaster Management and Risk Reduction Technology (CEDIM), Helmholtz Centre Potsdam, Telegrafenberg, 14473, Potsdam, Germany</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Luzi</subfield>
   <subfield code="D">L.</subfield>
   <subfield code="u">Sezione di Milano Pavia, Istituto Nazionale di Geofisica e Vulcanologia, Via Bassini 15, 20133, Milan, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Parolai</subfield>
   <subfield code="D">S.</subfield>
   <subfield code="u">GFZ German Research Centre for Geosciences, Centre for Disaster Management and Risk Reduction Technology (CEDIM), Helmholtz Centre Potsdam, Telegrafenberg, 14473, Potsdam, Germany</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Di Giacomo</subfield>
   <subfield code="D">D.</subfield>
   <subfield code="u">GFZ German Research Centre for Geosciences, Centre for Disaster Management and Risk Reduction Technology (CEDIM), Helmholtz Centre Potsdam, Telegrafenberg, 14473, Potsdam, Germany</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Monachesi</subfield>
   <subfield code="D">G.</subfield>
   <subfield code="u">Centro Nazionale Terremoti, Istituto Nazionale di Geofisica e Vulcanologia, Ancona, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="773" ind1="0" ind2=" ">
   <subfield code="t">Bulletin of Earthquake Engineering</subfield>
   <subfield code="d">Springer Netherlands</subfield>
   <subfield code="g">9/6(2011-12-01), 1941-1959</subfield>
   <subfield code="x">1570-761X</subfield>
   <subfield code="q">9:6&lt;1941</subfield>
   <subfield code="1">2011</subfield>
   <subfield code="2">9</subfield>
   <subfield code="o">10518</subfield>
  </datafield>
  <datafield tag="856" ind1="4" ind2="0">
   <subfield code="u">https://doi.org/10.1007/s10518-011-9273-3</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="908" ind1=" " ind2=" ">
   <subfield code="D">1</subfield>
   <subfield code="a">research-article</subfield>
   <subfield code="2">jats</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">856</subfield>
   <subfield code="E">40</subfield>
   <subfield code="u">https://doi.org/10.1007/s10518-011-9273-3</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Bindi</subfield>
   <subfield code="D">D.</subfield>
   <subfield code="u">GFZ German Research Centre for Geosciences, Centre for Disaster Management and Risk Reduction Technology (CEDIM), Helmholtz Centre Potsdam, Telegrafenberg, 14473, Potsdam, Germany</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Luzi</subfield>
   <subfield code="D">L.</subfield>
   <subfield code="u">Sezione di Milano Pavia, Istituto Nazionale di Geofisica e Vulcanologia, Via Bassini 15, 20133, Milan, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Parolai</subfield>
   <subfield code="D">S.</subfield>
   <subfield code="u">GFZ German Research Centre for Geosciences, Centre for Disaster Management and Risk Reduction Technology (CEDIM), Helmholtz Centre Potsdam, Telegrafenberg, 14473, Potsdam, Germany</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Di Giacomo</subfield>
   <subfield code="D">D.</subfield>
   <subfield code="u">GFZ German Research Centre for Geosciences, Centre for Disaster Management and Risk Reduction Technology (CEDIM), Helmholtz Centre Potsdam, Telegrafenberg, 14473, Potsdam, Germany</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Monachesi</subfield>
   <subfield code="D">G.</subfield>
   <subfield code="u">Centro Nazionale Terremoti, Istituto Nazionale di Geofisica e Vulcanologia, Ancona, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">773</subfield>
   <subfield code="E">0-</subfield>
   <subfield code="t">Bulletin of Earthquake Engineering</subfield>
   <subfield code="d">Springer Netherlands</subfield>
   <subfield code="g">9/6(2011-12-01), 1941-1959</subfield>
   <subfield code="x">1570-761X</subfield>
   <subfield code="q">9:6&lt;1941</subfield>
   <subfield code="1">2011</subfield>
   <subfield code="2">9</subfield>
   <subfield code="o">10518</subfield>
  </datafield>
  <datafield tag="900" ind1=" " ind2="7">
   <subfield code="a">Metadata rights reserved</subfield>
   <subfield code="b">Springer special CC-BY-NC licence</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="898" ind1=" " ind2=" ">
   <subfield code="a">BK010053</subfield>
   <subfield code="b">XK010053</subfield>
   <subfield code="c">XK010000</subfield>
  </datafield>
  <datafield tag="949" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="F">NATIONALLICENCE</subfield>
   <subfield code="b">NL-springer</subfield>
  </datafield>
 </record>
</collection>
