<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
<record>
  <controlfield tag="001">7393</controlfield>
  <controlfield tag="005">20250122113220.0</controlfield>
  <datafield tag="037" ind1=" " ind2=" ">
    <subfield code="a">POSTER-2025-0030</subfield>
  </datafield>
  <datafield tag="100" ind1=" " ind2=" ">
    <subfield code="a">Torres-Orozco, Rafael</subfield>
  </datafield>
  <datafield tag="245" ind1=" " ind2=" ">
    <subfield code="a">Combined pyroclast microtextures and seismic noise records demonstrate shallow andesite magma decompression drives different PDC mechanisms at Volcán de Colima, Mexico</subfield>
  </datafield>
  <datafield tag="260" ind1=" " ind2=" ">
    <subfield code="c">2023</subfield>
  </datafield>
  <datafield tag="269" ind1=" " ind2=" ">
    <subfield code="c">2023-12-11</subfield>
  </datafield>
  <datafield tag="520" ind1=" " ind2=" ">
    <subfield code="a">Volcán de Colima, the most active andesitic stratovolcano in Mexico, last erupted explosively on July 10-11, 2015, producing pyroclastic density currents (PDCs) of different type. The July-10 PDCs formed dense block-and-ash flow deposits typical of Volcán de Colima's history of recurrent summit dome effusion and collapse. In contrast, the July-11 PDCs comprised hot and turbulent scoria-rich PDCs that were unforeseen, and whose triggers and precursors were unidentified. Here, chemical and microtextural analyses of the July-11 deposits via electron-microscopy and x-rays microtomography revealed that decompression of andesite magma at fluctuating rates (10-3-100 MPa s-1) from 2 km-depth triggered magma degassing and crystallization. The resulting extremely rheologically heterogeneous magma fragmented and powered the pulsating July-11 PDCs that released 100-300 m3 s-1 on surface. Seismic noise velocity variations identified in each day down to 2 km-depth support magma decompression from a shallow reservoir. The combined geological and seismological evidence suggest timescales of only hours to couple of days from conduit and dome cracking and collapse to magma decompression and eruption.</subfield>
  </datafield>
  <datafield tag="594" ind1=" " ind2=" ">
    <subfield code="a">NO</subfield>
  </datafield>
  <datafield tag="653" ind1="1" ind2=" ">
    <subfield code="a">Volcanology</subfield>
  </datafield>
  <datafield tag="653" ind1="1" ind2=" ">
    <subfield code="a">Eruption</subfield>
  </datafield>
  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">De Plaen, Raphael</subfield>
  </datafield>
  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Capra, Lucia</subfield>
  </datafield>
  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Marquez, Victor H.</subfield>
  </datafield>
  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Sulpizio, Roberto</subfield>
  </datafield>
  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Arambula, Raúl</subfield>
  </datafield>
  <datafield tag="773" ind1=" " ind2=" ">
    <subfield code="t">AGU Fall Meeting, San Francisco</subfield>
  </datafield>
  <datafield tag="856" ind1="0" ind2=" ">
    <subfield code="f">raphael.deplaen@ksb-orb.be</subfield>
  </datafield>
  <datafield tag="856" ind1="4" ind2="2">
    <subfield code="a">https://ui.adsabs.harvard.edu/abs/2023AGUFM.V13B0111T/abstract</subfield>
  </datafield>
  <datafield tag="980" ind1=" " ind2=" ">
    <subfield code="a">CPOSTER</subfield>
  </datafield>
</record>
</collection>