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    <subfield code="a">CD I116 64 0015469</subfield>
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    <subfield code="a">Sedimentolog&#xED;a y perfiles de rayos gamma de la formaci&#xF3;n pozo D-129 (aptiano) en la Sierra de San Bernardo, Chubut</subfield>
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    <subfield code="a">10/11/2016 ; 10/11/2016</subfield>
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    <subfield code="a">25 p.</subfield>
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    <subfield code="a">Sedimentology and gamma-ray logs of the Pozo D-129 formation (Aptian) in the Sierra de San Bernardo, Chubut The study provides an outcrop analogue of productive hydrocarbon succesions of the uppermost part of the Pozo D-129 formation (Aptian) in the Golfo San Jorge basin. Although widely distributed in the subsurface of the basin, the Pozo D-129 formation is just exposed in three areas of the San Bernardo Fold Belt; this contribution presents the result of a sedimentological analysis carried out in the Sierra Silva (43 m thick) and Codo del Senguerr (140 m thick) anticlines. Facies analysis allowed the identification of thirteen lithofacies, which were grouped in three main lithofacies associations: (A) deep lacustrine, (B) sub-litoral lacustrine, and (C) shallow lacustrine. The later association consists of four sub-associations: C1 (carbonatic lake), C2 (distributary channels), C3 (distributary mouth bar) and C4 (interdistributary bay). Incomplete shallowing-upward cycles are common in both study areas, evidencing sedimentary progradation. Total and spectral gamma-ray (GR) measurements were obtained using a hand-held device. In Sierra Silva the shape of the U and total GR logs is similar, reflecting that minerals containing U are responsible of most of the emissions of this rocks; diagenetic enrichment of U occurred in a 4,5 m thick section, with measurements up to 500 ppm of U (378 g/tn de U3O8). At Codo del Senguerr, Th and K measurements in fine-grained rocks display better correlation with the total GR log than U, evidencing a different source of radioactive minerals. Integration of sedimentology and gammaray measurements bring data and lithological correspondences that could be useful for regional correlations and subsurface facies models.</subfield>
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    <subfield code="a">Paredes, Jos&#xE9; M.</subfield>
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    <subfield code="a">Allard, Jos&#xE9; O.</subfield>
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    <subfield code="a">Foix, Nicol&#xE1;s</subfield>
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    <subfield code="a">&#xC1;lvarez, Bruno</subfield>
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    <subfield code="a">Olaz&#xE1;bal, Sabrina X.</subfield>
    <subfield code="9">55751</subfield>
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    <subfield code="a">Congreso de Exploraci&#xF3;n y Desarrollo de Hidrocarburos (9no. : 2014 nov. 3-7 : Mendoza)</subfield>
    <subfield code="9">54287</subfield>
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    <subfield code="u">https://biblioteca.iapg.org.ar/ArchivosAdjuntos/CONEXPLOR2014/455-Sedimentologiayperfiles.pdf</subfield>
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    <subfield code="a">BAAB</subfield>
    <subfield code="b">BAAB</subfield>
    <subfield code="c">CD I116 64 0015469</subfield>
    <subfield code="d">2026-03-06</subfield>
    <subfield code="j">200062070</subfield>
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    <subfield code="o">CD I116 64 0015469</subfield>
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    <subfield code="r">2026-03-06 00:19:59</subfield>
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