Evidencias de paragénesis en cuevas kársticas de la vertiente cantábrica (norte de la Península Ibérica)

• Martin Arriolabengoa ^[1] ; D. Ballesteros ^[4] ; I. Álvarez ^[1] ; A. Aranburu ^[1] ; P. Bilbao ^[1] ; M. del Val ^[1] ; E. Iriarte ^[2] ; M. Jiménez-Sánchez ^[3]
  1. [1] Universidad del País Vasco/Euskal Herriko Unibertsitatea

     Universidad del País Vasco/Euskal Herriko Unibertsitatea

     Leioa, España

     
  2. [2] Universidad de Burgos

     Universidad de Burgos

     Burgos, España

     
  3. [3] Universidad de Oviedo

     Universidad de Oviedo

     Oviedo, España

     
  4. [4] Université de Rouen-Normandie y CNRS

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• Localización: XV Reunión Nacional de Cuaternario Bizkaia Aretoa: Bilbao, 1-5 julio 2019. Libro de resúmenes, 2019, ISBN 978-84-17713-16-4, págs. 152-155
• Idioma: español
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• Resumen

  • Paragenetic process regarding speleogenesis is globally accepted and recognised, but still few studies have established its importance in cave enlargement. Along the Cantabrian Margin (northern Iberian Peninsula), research developed during the last decade reported many paragenetic forms. In the present work, firstly, we compile documented paragenetic evidences in caves of the Cantabrian Margin in order to prove that paragenesis could be a relevant process in cave enlargement in this area. Secondly, we analyse possible factors that would favour the paragenesis. We conclude that this process is more extended in the development of Cantabrian karstic systems than expected until now