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  <controlfield tag="008">260224s        xxu                      </controlfield>
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    <subfield code="a">068.82 553.28 C62 15730</subfield>
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    <subfield code="a">De Simone, Hern&#xE1;n</subfield>
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    <subfield code="a">Pot&#xE1;s, Gustavo</subfield>
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  <datafield tag="111" ind1="2" ind2=" ">
    <subfield code="a">Congreso de Exploraci&#xF3;n y Desarrollo de Hidrocarburos (11er : 2022 nov. 8 - 11 : Mendoza)</subfield>
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  <datafield tag="245" ind1="0" ind2="0">
    <subfield code="a">CARACTERIZACI&#xD3;N S&#xCD;SMICA DE RESERVORIOS EN LA SERIE TOB&#xCD;FERA, MEDIANTE MODELADO DE CU&#xD1;A E INVERSI&#xD3;N DE TRAZAS. YACIMIENTO CA&#xD1;AD&#xD3;N PIEDRAS, CUENCA AUSTRAL, ARGENTINA</subfield>
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    <subfield code="a">18/08/2023 ; 18/08/2023</subfield>
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    <subfield code="a">12 p. ; 567-578</subfield>
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    <subfield code="a">A wedge model by simulating several thicknesses between Springhill Formation and Serie Tob&#xED;fera was made in the Ca&#xF1;ad&#xF3;n Piedras Field, in northern Tierra del Fuego, Austral Basin. The purpose of this work is to evaluate the seismic response in post and pre-stack domains, related to the changes in the thickness of the Formation. This is significantly important since it is intended to identify regions where the Springhill Fm. presents low or zero thickness (altos pelados), are propitious to develop reservoir conditions in volcanic intervals. They may also help to explain the charge with hydrocarbons through the sandy facies acting as carriers. So, it is key to develop tools to map wedging of Springhill Fm. to identify associated zones with good reservoir conditions in the Tob&#xED;fera Series. The results of the study through the interpretation of the values of P-Impedance allowed to discriminate and map the limits of the Springhill Fm. and the Tob&#xED;fera Series, as well as to outline internal geometries in both intervals. It was observed that high impedance values correspond to lithologies of greater hardness and low chances of presenting good reservoir properties, while low impedance values are associated with less solid lithologies and with possibilities of presenting some type of porosity.</subfield>
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    <subfield code="u">https://biblioteca.iapg.org.ar/ArchivosArchivosAdjuntos/Conexplor2022/Geof&#xED;sica/geofisica31.pdf</subfield>
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  <datafield tag="945" ind1=" " ind2=" ">
    <subfield code="a">Dominguez, Silvia</subfield>
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  <datafield tag="999" ind1=" " ind2=" ">
    <subfield code="c">196030</subfield>
    <subfield code="d">196030</subfield>
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    <subfield code="a">BVIAPG</subfield>
    <subfield code="b">BVIAPG</subfield>
    <subfield code="d">2026-03-06</subfield>
    <subfield code="l">0</subfield>
    <subfield code="o">068.82 553.28 C62 15730</subfield>
    <subfield code="p">200068448</subfield>
    <subfield code="r">2026-03-06 00:41:25</subfield>
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