<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
 <record>
  <leader>     caa a22        4500</leader>
  <controlfield tag="001">445846984</controlfield>
  <controlfield tag="003">CHVBK</controlfield>
  <controlfield tag="005">20180317145402.0</controlfield>
  <controlfield tag="007">cr unu---uuuuu</controlfield>
  <controlfield tag="008">170323e20110601xx      s     000 0 eng  </controlfield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">10.1007/s10518-011-9263-5</subfield>
   <subfield code="2">doi</subfield>
  </datafield>
  <datafield tag="035" ind1=" " ind2=" ">
   <subfield code="a">(NATIONALLICENCE)springer-10.1007/s10518-011-9263-5</subfield>
  </datafield>
  <datafield tag="245" ind1="0" ind2="0">
   <subfield code="a">Site effects &quot;on the rock”: the case of Castelvecchio Subequo (L'Aquila, central Italy)</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[S. Marzorati, C. Ladina, E. Falcucci, S. Gori, M. Saroli, G. Ameri, F. Galadini]</subfield>
  </datafield>
  <datafield tag="520" ind1="3" ind2=" ">
   <subfield code="a">The April 6, 2009 L'Aquila earthquake was responsible for an &quot;anomalous”, relatively high degree of damage (i.e. Is 7 MCS scale) at Castelvecchio Subequo (CS). Indeed, the village is located at source-to-site distance of about 40km, and it is surrounded by other inhabited centres to which considerably lower intensities, i.e. Is 5-6, have been attributed. Moreover, the damage was irregularly distributed within CS, being mainly concentrated in the uppermost portion of the old village. Geophysical investigations (ambient seismic noise and weak ground motions analyses) revealed that site effects occurred at CS. Amplifications of the ground motion, mainly striking NE-SW, have been detected at the uppermost portion of the carbonate ridge on which the village is built. Geological/structural and geomechanical field surveys defined that the CS ridge is affected by sets of fractures, joints and shear planes—mainly roughly NW-SE and N-S trending—that are related to the deformation zone of the Subequana valley fault system and to transfer faults linking northward the mentioned tectonic feature with the Middle Aterno Valley fault system. In particular, our investigations highlight that seismic amplifications occur where joints set NW-SE trending are open. On the other hand, no amplification is seen in portions of the ridge where the bedrock is densely fractured but no open joints occur. The fracture opening seems related to the toppling tendency of the bedrock slabs, owing to the local geomorphic setting. These investigations suggest that the detected amplification of the ground motion is probably related to the polarization of the seismic waves along the Castelvecchio Subequo ridge, with the consequent oscillation of the rock slabs perpendicularly to the fractures azimuth.</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">Rock sites</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Spectral ratios</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Ambient seismic noise</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Structural characteristics</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Jointing conditions</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Geomechanical analysis</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">2009 L'Aquila earthquake</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Central Italy</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Marzorati</subfield>
   <subfield code="D">S.</subfield>
   <subfield code="u">Centro Nazionale Terremoti Sede di Ancona, Istituto Nazionale di Geofisica e Vulcanologia, Strada Cameranense 1, 60131, Passo Varano, AN, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Ladina</subfield>
   <subfield code="D">C.</subfield>
   <subfield code="u">Centro Nazionale Terremoti Sede di Ancona, Istituto Nazionale di Geofisica e Vulcanologia, Strada Cameranense 1, 60131, Passo Varano, AN, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Falcucci</subfield>
   <subfield code="D">E.</subfield>
   <subfield code="u">Sezione di Roma1, Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Gori</subfield>
   <subfield code="D">S.</subfield>
   <subfield code="u">Sezione di Roma1, Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Saroli</subfield>
   <subfield code="D">M.</subfield>
   <subfield code="u">Dipartimento di Meccanica, Strutture, Ambiente e Territorio, Università di Cassino, Cassino, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Ameri</subfield>
   <subfield code="D">G.</subfield>
   <subfield code="u">Sezione di Milano-Pavia, Istituto Nazionale di Geofisica e Vulcanologia, Milan, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Galadini</subfield>
   <subfield code="D">F.</subfield>
   <subfield code="u">Sezione di Roma1, Istituto Nazionale di Geofisica e Vulcanologia, Rome, 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">9/3(2011-06-01), 841-868</subfield>
   <subfield code="x">1570-761X</subfield>
   <subfield code="q">9:3&lt;841</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/s10518-011-9263-5</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/s10518-011-9263-5</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">Marzorati</subfield>
   <subfield code="D">S.</subfield>
   <subfield code="u">Centro Nazionale Terremoti Sede di Ancona, Istituto Nazionale di Geofisica e Vulcanologia, Strada Cameranense 1, 60131, Passo Varano, AN, 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">Ladina</subfield>
   <subfield code="D">C.</subfield>
   <subfield code="u">Centro Nazionale Terremoti Sede di Ancona, Istituto Nazionale di Geofisica e Vulcanologia, Strada Cameranense 1, 60131, Passo Varano, AN, 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">Falcucci</subfield>
   <subfield code="D">E.</subfield>
   <subfield code="u">Sezione di Roma1, Istituto Nazionale di Geofisica e Vulcanologia, Rome, 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">Gori</subfield>
   <subfield code="D">S.</subfield>
   <subfield code="u">Sezione di Roma1, Istituto Nazionale di Geofisica e Vulcanologia, Rome, 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">Saroli</subfield>
   <subfield code="D">M.</subfield>
   <subfield code="u">Dipartimento di Meccanica, Strutture, Ambiente e Territorio, Università di Cassino, Cassino, 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">Ameri</subfield>
   <subfield code="D">G.</subfield>
   <subfield code="u">Sezione di Milano-Pavia, Istituto Nazionale di Geofisica e Vulcanologia, 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">Galadini</subfield>
   <subfield code="D">F.</subfield>
   <subfield code="u">Sezione di Roma1, Istituto Nazionale di Geofisica e Vulcanologia, Rome, 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">9/3(2011-06-01), 841-868</subfield>
   <subfield code="x">1570-761X</subfield>
   <subfield code="q">9:3&lt;841</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>
