<?xml version="1.0" encoding="UTF-8"?>
<record
    xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance"
    xsi:schemaLocation="http://www.loc.gov/MARC21/slim http://www.loc.gov/standards/marcxml/schema/MARC21slim.xsd"
    xmlns="http://www.loc.gov/MARC21/slim">

  <leader>02485nmc a2200277   4500</leader>
  <controlfield tag="005">20260520010405.0</controlfield>
  <controlfield tag="008">260224s2018    xxu                 esp  </controlfield>
  <datafield tag="041" ind1=" " ind2=" ">
    <subfield code="a">Espa&#xF1;ol</subfield>
  </datafield>
  <datafield tag="082" ind1=" " ind2=" ">
    <subfield code="a">068.82 553.28 C62 2018 0015658</subfield>
  </datafield>
  <datafield tag="245" ind1="0" ind2="0">
    <subfield code="a">La Formaci&#xF3;n Loma Montosa en el borde nororiental de la Cuenca Neuquina: An&#xE1;lisis secuencial, carcterizaci&#xF3;n paleoambiental y prospectividad remanente</subfield>
  </datafield>
  <datafield tag="260" ind1=" " ind2=" ">
    <subfield code="a"></subfield>
    <subfield code="b"></subfield>
    <subfield code="c">2018</subfield>
  </datafield>
  <datafield tag="270" ind1=" " ind2=" ">
    <subfield code="a">02/09/2025 ; 09/04/2019</subfield>
  </datafield>
  <datafield tag="300" ind1=" " ind2=" ">
    <subfield code="a">22 p. ; 623-645</subfield>
  </datafield>
  <datafield tag="520" ind1=" " ind2=" ">
    <subfield code="a">The understanding of stratigraphic frameworks and paleoenvironmental models constitute a key element to improve both exploration and development of oil and gas fields. A methodology that extended through a broad scale of analyses, going from regional seismic interpretation, to well log interpretation, and core and cutting characterization, allowed us to assign a carbonate-siliciclastic interval in the NE of the Neuquen Basin Platform to Intramalmic-Intravalanginian ages; additionally, this interval was defined as part of Loma Montosa Fm. The interpretation of facies associations both from core and cutting, and its vertical arrangement were used to define depositional trends, main stratigraphic surfaces, and finally develop an environmental evolution model of this cycle. The Loma Montosa Fm. in the studied zone is limited in its base by a regional transgressive surface and in its top by the Intravalanginian unconformity; at least two transgressive and one regressive lower hierarchy surfaces were also defined within this cycle. The carbonate-siliciclastic sequence assigned in this work to Loma Montosa is interpreted as a ramp or mixed shoreface with a very low structural gradient, in which grainstone deposits are defined as high energy coastal environments and could constitute a potential reservoir if adequate stimulation is applied. This would comprise a new play prospectable in a regional scale.</subfield>
  </datafield>
  <datafield tag="773" ind1=" " ind2=" ">
    <subfield code="g"></subfield>
  </datafield>
  <datafield tag="942" ind1=" " ind2=" ">
    <subfield code="c">CONGTP</subfield>
  </datafield>
  <datafield tag="100" ind1="1" ind2=" ">
    <subfield code="a">I&#xF1;igo, Juan Francisco Pedro</subfield>
    <subfield code="9">58794</subfield>
  </datafield>
  <datafield tag="100" ind1="1" ind2=" ">
    <subfield code="a">Vargas, Renzo</subfield>
    <subfield code="9">58795</subfield>
  </datafield>
  <datafield tag="100" ind1="1" ind2=" ">
    <subfield code="a">Novara, Eugenia</subfield>
    <subfield code="9">58796</subfield>
  </datafield>
  <datafield tag="100" ind1="1" ind2=" ">
    <subfield code="a">Pereira, Diego Martin</subfield>
    <subfield code="9">58797</subfield>
  </datafield>
  <datafield tag="100" ind1="1" ind2=" ">
    <subfield code="a">Schwarz, Ernesto</subfield>
    <subfield code="9">55713</subfield>
  </datafield>
  <datafield tag="111" ind1="2" ind2=" ">
    <subfield code="a">Congreso de Exploraci&#xF3;n y Desarrollo de Hidrocarburos (10mo. : 2018 nov. 5 - 9 : Mendoza)</subfield>
    <subfield code="9">573</subfield>
  </datafield>
  <datafield tag="650" ind1=" " ind2="0">
    <subfield code="a">Plataforma Nororiental Neuquina</subfield>
    <subfield code="9">58798</subfield>
  </datafield>
  <datafield tag="999" ind1=" " ind2=" ">
    <subfield code="c">192829</subfield>
    <subfield code="d">192829</subfield>
  </datafield>
  <datafield tag="856" ind1=" " ind2=" ">
    <subfield code="u">https://biblioteca.iapg.org.ar/ArchivosAdjuntos/Conexplor2018/1534.pdf</subfield>
  </datafield>
  <datafield tag="952" ind1=" " ind2=" ">
    <subfield code="0">0</subfield>
    <subfield code="1">0</subfield>
    <subfield code="4">0</subfield>
    <subfield code="7">0</subfield>
    <subfield code="9">260548</subfield>
    <subfield code="a">CDIAPG</subfield>
    <subfield code="b">CDIAPG</subfield>
    <subfield code="c">068.82 553.28 C62 2018 0015658</subfield>
    <subfield code="d">2026-03-06</subfield>
    <subfield code="j">200065132</subfield>
    <subfield code="l">0</subfield>
    <subfield code="o">068.82 553.28 C62 2018 0015658</subfield>
    <subfield code="p">200065132</subfield>
    <subfield code="r">2026-03-06 00:37:14</subfield>
    <subfield code="w">2026-03-06</subfield>
    <subfield code="y">ARCHIVO</subfield>
  </datafield>
</record>
