Las aguas subterráneas del Paisaje Protegido de la Sierra de Santo Domingo-Salinas(Pirineo Occidental)

  1. C. Oliván 1
  2. E.L. Pueyo 1
  3. E. Garrido-Schneider 1
  4. A. Azcón
  5. E.M. Sánchez-Moreno 2
  6. J.C. Larrasoaña 1
  7. F. Compaired 3
  1. 1 Instituto Geológico y Minero de España
    info

    Instituto Geológico y Minero de España

    Madrid, España

    ROR https://ror.org/04cadha73

  2. 2 Universidad de Burgos
    info

    Universidad de Burgos

    Burgos, España

    ROR https://ror.org/049da5t36

  3. 3 Gobierno de Aragón
    info

    Gobierno de Aragón

    Zaragoza, España

    ROR https://ror.org/0425pg203

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Revista:
Geotemas (Madrid)

ISSN: 1576-5172

Ano de publicación: 2021

Título do exemplar: X Congreso Geológico de España

Número: 18

Páxinas: 316

Tipo: Artigo

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Outras publicacións en: Geotemas (Madrid)

Resumo

The Santo Domingo-Salinas ranges represent the south-westernmost termination of the Pyrenean sole thrust separating the Pyrenees from the Ebro foreland basin to the South. The Santo Domingo anticline is the main structural feature in the area (Oliva-Urcia et al., 2012). This area practically lacks of hydrogeology studies. In this work, we provide a first hydrogeoche- mical characterization of the groundwater in the area. To do so, we have: i) compiled existing hydrogeological information, ii) exhaustively developed an inventory of water points, iii) sampled and analysed groundwaters and iv) interpreted the hydrochemical facies detected. The three aquifer systems defined by Garrido-Schneider (1995) have been improved. The most important one, the Santo Domingo-Salinas system, it is composed of Mesozoic and Cenozoic limestones formations. The che- mical analyses of groundwater allow us to differentiate four main types: a) calcium bicarbonate drained by limestones from the Cretaceous-Eocene aquifer, b) calcium-magnesium bicarbonate drained by limestones and dolomites from Muschelkalk facies (Triassic), c) calcium sulfate and d) sodium chloride, both related to siltstones and evaporites found within the Keuper facies (Triassic).

Fonte de datos: Dialnet