New insights on speleoseismology: The geothermal gradient and heat flow values in caves for the study of active faults

Author:

Pérez-López R.,Martín-Velázquez S.,Sánchez-Moral S.ORCID,Patyniak M.ORCID,López-Gutiérrez J.,Cuezva S.,Lario J.ORCID,Silva P.G.,Rodríguez-Pascua M.A.,Giner-Robles J.L.

Funder

MINECO-FEDER

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference45 articles.

1. The association between bubble trails and folia: a morphological and sedimentary indicator of hypogenic speleogenesis by degassing, example from Adaouste Cave (Provence, France);Audra;Int. J. Speleol.,2009

2. Crustal Heat Flow: a Guide to Measurement and Modelling;Beardsmore,2001

3. Speleoseismology: a critical perspective;Becker;J. Seismol.,2006

4. Modelling of speleothems failure in the Hotton Cave (Belgium). Is the failure earthquake induced?;Cadorin;Neth. J. Geosci.,2001

5. A cavity ring-down analyzer for measuring atmospheric levels of methane, carbon dioxide, and water vapor;Crosson;Appl. Phys. B Lasers Opt.,2008

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