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  <controlfield tag="008">260224s        xxu                      </controlfield>
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    <subfield code="a">Doiny Cabr&#xE9;, Juan Pedro</subfield>
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    <subfield code="a">Fumarola, Lara Azul</subfield>
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    <subfield code="a">Congreso de Exploraci&#xF3;n y Desarrollo de Hidrocarburos (11er : 2022 nov. 8 - 11 : Mendoza)</subfield>
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    <subfield code="a">CARACTERIZACI&#xD3;N Y MODELADO ESTRUCTURAL DE LOS ANTICLINALES CASHIRIARI Y SAN MART&#xCD;N EN LA FAJA PLEGADA Y CORRIDA DE CAMISEA, ANDES CENTRALES, PER&#xDA;</subfield>
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    <subfield code="a">15/08/2023 ; 15/08/2023</subfield>
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    <subfield code="a">The Camisea fold and thrust belt, located in the southern Ucayali Basin, has been extensively studied due to its important hydrocarbon accumulations. High-quality 3D depth-migrated seismic data allows the identifica-tion of five structural trends in a thin-skinned fold and thrust belt. The main structures are north-verging thrusts with a basal detachment that deepens southward. The San Martin and Cashiriari anticlines, which are the focus of this work, are interpreted as fault-bend folds. In order to analyze along-strike variations of these structures, four cross-sections were made. Besides the north-verging thrusts, high angle reverse faults with opposite vergence can be identified. The analysis of the crosscutting relationships between the different structures allows us to define a sequence of deformation in which the high angle reverse faults precede and are cut by the main north-verging thrusts. A kinematic evolution of the structure is presented in order to verify the correct restoration and validate the structural cross-section interpretation.</subfield>
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    <subfield code="u">https://biblioteca.iapg.org.ar/ArchivosAdjuntos/Conexplor2022/Geolog&#xED;aEstructural/geologia-estructural-y-tectonica15.PDF</subfield>
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    <subfield code="d">2026-03-06</subfield>
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    <subfield code="o">068.82 553.28 C62 15730</subfield>
    <subfield code="p">200068391</subfield>
    <subfield code="r">2026-03-06 00:41:19</subfield>
    <subfield code="y">ARCHIVO</subfield>
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