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  <controlfield tag="008">260224s2018    xxu                 esp  </controlfield>
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    <subfield code="a">Espa&#xF1;ol</subfield>
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    <subfield code="a">068.82 553.28 C62 2018 0015655</subfield>
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    <subfield code="a">Estratigraf&#xED;a de alta resoluci&#xF3;n y su implicancia para el modelado 3D de reservorios en la formaci&#xF3;n Lajas (Grupo Cuyo) -Anticlinal de Pic&#xFA;n Leuf&#xFA;- Cuenca Neuquina</subfield>
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    <subfield code="c">2018</subfield>
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  <datafield tag="270" ind1=" " ind2=" ">
    <subfield code="a">01/07/2022 ; 06/03/2019</subfield>
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    <subfield code="a">18 p. ; 295-313</subfield>
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    <subfield code="a">In the South part of the Neuqu&#xE9;n basin (Pic&#xFA;n Leuf&#xFA; anticline), the Jurassic deposits of the Lajas Formation have outcropping sections with very good state of preservation and high lateral continuities. These characteristics favor the use of these rocks as analogues for hydrocarbon reservoirs.Several previous researchers have studied this geological Formation. The section, constituted by fluvio-deltaic deposits, presents, according to others researchers, three sedimentary sequences of low frequency (3rd order). They also recognize a major regional unconformity (Intrabajocian) that is recognize over all the extensi&#xF3;n of the Huincul&amp;#x92;s Dorsal, between the first and second sequences, which divides the analyzed unit into two sections.The present work was carried out in the lower portion of the Lajas Formation below the mentioned regional unconformity. Two (predominantly progradational) sequences of low (&gt;8 km extension) and ten of medium (3-8 km) frequencies - corresponding to the previous 3rd and 4th orders - were described. The definition and mapping of high frequency sequences (&lt;300 m) is one of the contributions of this article. From the data collected in the 19 outcrop sections, the sedimentological and paleogeographic characterizations of the analyzed section were established. The stratigraphic framework defined and applicable to the study area is based on the individualization of medium frequency sequences and was very important for the preparation of 3D geological models.The stratigraphic analysis of the medium frequency sequences allowed identifying that the progradation of the deltaic system varied from 250 &#xB0; to 350 &#xB0;. The observation of the high frequency sequences enhance the understanding of vertical distribution and lateral extension of permeability barriers (fade out?) and sandy bodies (potential reservoirs).The results obtained from the simulations of facies, with different provided data (bibliographic vs. field-collected), showed qualitatively and quantitatively the degree of success that high-resolution stratigraphy can bring to 3D reservoir modeling and to its application in the optimization of hydrocarbon exploitation.</subfield>
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    <subfield code="c">CONGTP</subfield>
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  <datafield tag="100" ind1="1" ind2=" ">
    <subfield code="a">De Moraes Lima Silveira, Miguel</subfield>
    <subfield code="9">58473</subfield>
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  <datafield tag="100" ind1="1" ind2=" ">
    <subfield code="a">Arregui, Carlos Daniel</subfield>
    <subfield code="9">48414</subfield>
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  <datafield tag="100" ind1="1" ind2=" ">
    <subfield code="a">Pederneiras Raja Gabaglia, Guilherme</subfield>
    <subfield code="9">58474</subfield>
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  <datafield tag="100" ind1="1" ind2=" ">
    <subfield code="a">Veiga, Gonzalo Diego</subfield>
    <subfield code="9">58475</subfield>
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  <datafield tag="100" ind1="1" ind2=" ">
    <subfield code="a">Galvao Carnier Fragoso, Daniel</subfield>
    <subfield code="9">58476</subfield>
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  <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="111" ind1="2" ind2=" ">
    <subfield code="a">Simposio de Recursos No Convencionales (2018 nov. 5 - 9 : Mendoza)</subfield>
    <subfield code="9">781</subfield>
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  <datafield tag="650" ind1=" " ind2="0">
    <subfield code="a">Lajas</subfield>
    <subfield code="9">58477</subfield>
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  <datafield tag="650" ind1=" " ind2="0">
    <subfield code="a">Estratigraf&#xED;a</subfield>
    <subfield code="9">783</subfield>
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  <datafield tag="650" ind1=" " ind2="0">
    <subfield code="a">Reservorios</subfield>
    <subfield code="9">708</subfield>
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  <datafield tag="999" ind1=" " ind2=" ">
    <subfield code="c">192698</subfield>
    <subfield code="d">192698</subfield>
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  <datafield tag="856" ind1=" " ind2=" ">
    <subfield code="u">https://biblioteca.iapg.org.ar/ArchivosAdjuntos/Conexplor2018/SRNC/1278.pdf</subfield>
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    <subfield code="9">260417</subfield>
    <subfield code="a">CDIAPG</subfield>
    <subfield code="b">CDIAPG</subfield>
    <subfield code="c">068.82 553.28 C62 2018 0015655</subfield>
    <subfield code="d">2026-03-06</subfield>
    <subfield code="j">200065000</subfield>
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    <subfield code="o">068.82 553.28 C62 2018 0015655</subfield>
    <subfield code="p">200065000</subfield>
    <subfield code="r">2026-03-06 00:37:04</subfield>
    <subfield code="w">2026-03-06</subfield>
    <subfield code="y">ARCHIVO</subfield>
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