<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
 <record>
  <leader>     caa a22        4500</leader>
  <controlfield tag="001">463172345</controlfield>
  <controlfield tag="003">CHVBK</controlfield>
  <controlfield tag="005">20180406164817.0</controlfield>
  <controlfield tag="007">cr unu---uuuuu</controlfield>
  <controlfield tag="008">170326e20070401xx      s     000 0 eng  </controlfield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">10.1007/s10950-007-9048-0</subfield>
   <subfield code="2">doi</subfield>
  </datafield>
  <datafield tag="035" ind1=" " ind2=" ">
   <subfield code="a">(NATIONALLICENCE)springer-10.1007/s10950-007-9048-0</subfield>
  </datafield>
  <datafield tag="245" ind1="0" ind2="0">
   <subfield code="a">Variation of human perceptiveness of earthquakes during seismic sequences</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[Luigi Cucci, Andrea Tertulliani]</subfield>
  </datafield>
  <datafield tag="520" ind1="3" ind2=" ">
   <subfield code="a">This paper describes the variation of the human perception of earthquakes under the peculiar condition of seismic sequence occurrence. To this aim, we chose and have analyzed four seismic sequences that reflect the most common models of seismicity occurrence in the Italian territory. Our data always refer to the epicentral area, so that the contribution of the epicentral distance to the earthquake sensitiveness is considered constant. To search for recurrent behavior of people in the perception of earthquakes, we crossed seismological data to sensitivity data coming from the archives of the Italian Civil Protection. In each sequence, we individuate a number of &quot;indicators”, such as the rate between felt and not-felt events and the minimum magnitude for which 100% of the events are felt. Such indicators are proportional to the energy released by the sequence and can be particularly affected by the time protraction of the sequence, and/or by the different familiarity with the seismic phenomenon, and/or by the intensity of the emotional impact of a seismic crisis. The observed trends of sensitiveness show a significant variation of the people perceptivity within the sequence development. From the analysis of the dataset, one can distinguish the variation of perceptivity due to emotional factors from those due to physical factors. An important observation, which is confirmed by a statistical analysis, is that the source depth does not affect the perceptiveness of earthquakes. Finally, we find important differences between on-sequence and off-sequence human perceptiveness that are connected with the different levels of alert.</subfield>
  </datafield>
  <datafield tag="540" ind1=" " ind2=" ">
   <subfield code="a">Springer Science+Business Media, Inc., 2007</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">seismic sequence</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">magnitude</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">perceptiveness</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">human reaction</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Cucci</subfield>
   <subfield code="D">Luigi</subfield>
   <subfield code="u">Istituto Nazionale di Geofisica e Vulcanologia, Via di Vigna Murata 605, 00147, Rome, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Tertulliani</subfield>
   <subfield code="D">Andrea</subfield>
   <subfield code="u">Istituto Nazionale di Geofisica e Vulcanologia, Via di Vigna Murata 605, 00147, Rome, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="773" ind1="0" ind2=" ">
   <subfield code="t">Journal of Seismology</subfield>
   <subfield code="d">Kluwer Academic Publishers</subfield>
   <subfield code="g">11/2(2007-04-01), 205-219</subfield>
   <subfield code="x">1383-4649</subfield>
   <subfield code="q">11:2&lt;205</subfield>
   <subfield code="1">2007</subfield>
   <subfield code="2">11</subfield>
   <subfield code="o">10950</subfield>
  </datafield>
  <datafield tag="856" ind1="4" ind2="0">
   <subfield code="u">https://doi.org/10.1007/s10950-007-9048-0</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/s10950-007-9048-0</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">Cucci</subfield>
   <subfield code="D">Luigi</subfield>
   <subfield code="u">Istituto Nazionale di Geofisica e Vulcanologia, Via di Vigna Murata 605, 00147, 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">Tertulliani</subfield>
   <subfield code="D">Andrea</subfield>
   <subfield code="u">Istituto Nazionale di Geofisica e Vulcanologia, Via di Vigna Murata 605, 00147, 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">Journal of Seismology</subfield>
   <subfield code="d">Kluwer Academic Publishers</subfield>
   <subfield code="g">11/2(2007-04-01), 205-219</subfield>
   <subfield code="x">1383-4649</subfield>
   <subfield code="q">11:2&lt;205</subfield>
   <subfield code="1">2007</subfield>
   <subfield code="2">11</subfield>
   <subfield code="o">10950</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>
