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handle: 10261/273690
Hidrográficamente, los Bajos Submeridionales (BBSS) forman parte de la cuenca media e inferior del río Salado, afluente del río Paraná, en la que existen numerosos cuerpos de agua superficial permanentes o semipermanentes que ocupan hoyas de deflación presentes en la suave pendiente regional, característica de las grandes llanuras. Los BBSS forman parte de una gran cuenca sedimentaria que sobrepasa los 5.000 metros de espesor, calculados por sísmica (Pezzi y Mozetic, 1989) y está emplazada sobre rocas de edades paleoproterozoicas (Rapela et al., 2007).
Centro de Estudios Hidro-Ambientales, Universidad Nacional del Litoral, Argentina
Facultad de Ciencias Agrarias, Universidad Nacional de Entre Ríos, Argentina
Consejo Nacional de Investigaciones Científicas y Técnicas, Argentina
Centro Regional Litoral, Instituto Nacional del Agua, Argentina
Congreso nacional del agua (26º. 2017. Córdoba, Argentina)
Instituto Geológico y Minero de España, España
Peer reviewed
Geomorfología, Hidrogeología, Argentina, Geología
Geomorfología, Hidrogeología, Argentina, Geología
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