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</o:shapelayout></xml><![endif]--></head><body lang=es-419 link="#0563C1" vlink="#954F72" style='word-wrap:break-word'><div class=WordSection1><h1 style='mso-margin-top-alt:0cm;margin-right:0cm;margin-bottom:15.0pt;margin-left:0cm;line-height:22.5pt;background:white'><span style='font-size:18.0pt;font-family:"Noto Sans",sans-serif;color:#203864;mso-style-textfill-fill-color:#203864;mso-style-textfill-fill-alpha:100.0%'><span style='color:windowtext'>Revista de la Asociación Geológica Argentina Vol. 78 Núm. 4 (2021)<o:p></o:p></span></span></h1><h2 style='mso-margin-top-alt:0cm;margin-right:0cm;margin-bottom:15.0pt;margin-left:0cm;line-height:22.5pt;background:white'><span style='font-size:12.0pt;font-family:"Noto Sans",sans-serif;color:black;font-weight:normal'>Artículos</span><span style='font-size:12.0pt;font-family:"Noto Sans",sans-serif;font-weight:normal'><o:p></o:p></span></h2><h3 style='mso-margin-top-alt:0cm;margin-right:0cm;margin-bottom:0cm;margin-left:36.0pt;text-indent:-18.0pt;line-height:15.0pt;mso-list:l1 level1 lfo1;background:white;box-sizing: border-box'><![if !supportLists]><span style='font-size:10.0pt;font-family:Symbol;font-weight:normal'><span style='mso-list:Ignore'>·<span style='font:7.0pt "Times New Roman"'> </span></span></span><![endif]><span style='font-size:10.5pt;font-family:"Noto Sans",sans-serif;color:black'><a href="https://revista.geologica.org.ar/raga/article/view/247"><span style='color:#007AB2'>Estratigrafía de la sucesión neógena en el Bolsón de Fiambalá, Sistema de Famatina, Catamarca, Argentina</span></a></span><span style='font-size:10.5pt;font-family:"Noto Sans",sans-serif'><o:p></o:p></span></h3><p class=MsoNormal style='mso-margin-top-alt:auto;margin-left:36.0pt;line-height:15.0pt;background:white'><span style='font-size:10.0pt;font-family:"Noto Sans",sans-serif;color:black'>Maximiliano Deri, Patricia Ciccioli, Sergio Marenssi, William Amidon</span><span style='font-size:10.0pt;font-family:"Noto Sans",sans-serif'><o:p></o:p></span></p><h3 style='mso-margin-top-alt:0cm;margin-right:0cm;margin-bottom:0cm;margin-left:36.0pt;line-height:15.0pt;background:white'><span style='font-size:10.5pt;font-family:"Noto Sans",sans-serif'><o:p> </o:p></span></h3><h3 style='mso-margin-top-alt:0cm;margin-right:0cm;margin-bottom:0cm;margin-left:36.0pt;text-indent:-18.0pt;line-height:15.0pt;mso-list:l1 level1 lfo1;background:white'><![if !supportLists]><span style='font-size:10.0pt;font-family:Symbol;font-weight:normal'><span style='mso-list:Ignore'>·<span style='font:7.0pt "Times New Roman"'> </span></span></span><![endif]><span style='font-size:10.5pt;font-family:"Noto Sans",sans-serif;color:black'><a href="https://revista.geologica.org.ar/raga/article/view/515"><span style='color:#007AB2'>Revisión estratigráfica y evolución paleoambiental del mesozoico temprano al sureste de la provincia de San Juan, Argentina</span></a></span><span style='font-size:10.5pt;font-family:"Noto Sans",sans-serif'><o:p></o:p></span></h3><p class=MsoNormal style='mso-margin-top-alt:auto;margin-left:36.0pt;line-height:15.0pt;background:white'><span style='font-size:10.0pt;font-family:"Noto Sans",sans-serif;color:black'>Carina Colombi, Paula Santi Malnis, Ricardo N. Martínez, Juan Drovandi, Gustavo Correa, Tatiana Soria</span><span style='font-size:10.0pt;font-family:"Noto Sans",sans-serif'><o:p></o:p></span></p><h3 style='mso-margin-top-alt:0cm;margin-right:0cm;margin-bottom:0cm;margin-left:36.0pt;line-height:15.0pt;background:white'><span style='font-size:10.5pt;font-family:"Noto Sans",sans-serif'><o:p> </o:p></span></h3><h3 style='mso-margin-top-alt:0cm;margin-right:0cm;margin-bottom:0cm;margin-left:36.0pt;text-indent:-18.0pt;line-height:15.0pt;mso-list:l1 level1 lfo1;background:white'><![if !supportLists]><span style='font-size:10.0pt;font-family:Symbol;font-weight:normal'><span style='mso-list:Ignore'>·<span style='font:7.0pt "Times New Roman"'> </span></span></span><![endif]><span style='font-size:10.5pt;font-family:"Noto Sans",sans-serif;color:black'><a href="https://revista.geologica.org.ar/raga/article/view/941"><span style='color:#007AB2'>Estudios de fábrica magnética en modelos análogos: comparación entre distintas mineralogías</span></a></span><span style='font-size:10.5pt;font-family:"Noto Sans",sans-serif'><o:p></o:p></span></h3><p class=MsoNormal style='mso-margin-top-alt:auto;margin-left:36.0pt;line-height:15.0pt;background:white'><span style='font-size:10.0pt;font-family:"Noto Sans",sans-serif;color:black'>Juan Martín Calvagno, María Belén Febbo, Renata Nela Tomezzoli, Leandro César Gallo, Ernesto Osvaldo Cristallini</span><span style='font-size:10.0pt;font-family:"Noto Sans",sans-serif'><o:p></o:p></span></p><h3 style='mso-margin-top-alt:0cm;margin-right:0cm;margin-bottom:0cm;margin-left:36.0pt;line-height:15.0pt;background:white'><span style='font-size:10.5pt;font-family:"Noto Sans",sans-serif'><o:p> </o:p></span></h3><h3 style='mso-margin-top-alt:0cm;margin-right:0cm;margin-bottom:0cm;margin-left:36.0pt;text-indent:-18.0pt;line-height:15.0pt;mso-list:l1 level1 lfo1;background:white'><![if !supportLists]><span style='font-size:10.0pt;font-family:Symbol;font-weight:normal'><span style='mso-list:Ignore'>·<span style='font:7.0pt "Times New Roman"'> </span></span></span><![endif]><span style='font-size:10.5pt;font-family:"Noto Sans",sans-serif;color:black'><a href="https://revista.geologica.org.ar/raga/article/view/214"><span style='color:#007AB2'>Evidencias de actividad cuaternaria asociadas a la falla La Aguada, piedemonte occidental de la sierra de Comechingones. 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Cuenca Río Blanco, Andes Centrales de Argentina</span></a></span><span style='font-size:10.5pt;font-family:"Noto Sans",sans-serif'><o:p></o:p></span></h3><p class=MsoNormal style='mso-margin-top-alt:auto;margin-left:36.0pt;line-height:15.0pt;background:white'><span style='font-size:10.0pt;font-family:"Noto Sans",sans-serif;color:black'>Maria Yanina Esper Angillieri, Ana Paula FORTE, Raúl Emmanuel OCAÑA, Cristian Daniel VILLARROEL</span><span style='font-size:10.0pt;font-family:"Noto Sans",sans-serif'><o:p></o:p></span></p><h3 style='mso-margin-top-alt:0cm;margin-right:0cm;margin-bottom:0cm;margin-left:36.0pt;line-height:15.0pt;background:white'><span style='font-size:10.5pt;font-family:"Noto Sans",sans-serif'><o:p> </o:p></span></h3><h3 style='mso-margin-top-alt:0cm;margin-right:0cm;margin-bottom:0cm;margin-left:36.0pt;text-indent:-18.0pt;line-height:15.0pt;mso-list:l1 level1 lfo1;background:white'><![if !supportLists]><span style='font-size:10.0pt;font-family:Symbol;font-weight:normal'><span style='mso-list:Ignore'>·<span style='font:7.0pt "Times New Roman"'> </span></span></span><![endif]><span style='font-size:10.5pt;font-family:"Noto Sans",sans-serif;color:black'><a href="https://revista.geologica.org.ar/raga/article/view/942"><span style='color:#007AB2'>Procesos de remoción en masa asociados a cuencas como base para la selección de alternativas de un camino de montaña. 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