New insights on speleoseismology: The geothermal gradient and heat flow values in caves for the study of active faults
Author:
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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1. Temperature variation in caves and its significance for subterranean ecosystems;Scientific Reports;2023-11-25
2. Radon concentration in caves as a proxy for tectonic activity in The Cantabrian Mountains (Spain);Acta Carsologica;2021-05-31
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