EarthRef.org Reference Database (ERR)
Development and Maintenance by the EarthRef.org Database Team

Detailed Reference Information
Charmoille et al. 2005
Charmoille, A., Fabbri, O., Mudry, J., Guglielmi, Y. and Bertrand, C. (2005). Post-seismic permeability change in a shallow fractured aquifer following a ML 5.1 earthquake (Fourbanne karst aquifer, Jura outermost thrust unit, eastern France). Geophysical Research Letters 32: doi: 10.1029/2005GL023859. issn: 0094-8276.

Following a ML 5.1 earthquake in eastern France, a post-seismic 12-day long electrical conductivity increase was recorded in the water discharging from a karst aquifer located 3 km from the epicentre. We attribute this to a permeability enhancement which allowed long-residence time water from low-permeability fractures located in the saturated zone to be expelled. The permeability enhancement shows that shallow aquifers can be significantly deformed for several days by moderate magnitude earthquakes.

BACKGROUND DATA FILES

Abstract

Keywords
Hydrology, Groundwater hydrology, Hydrology, Chemistry of fresh water, Seismology, Earthquake interaction, forecasting, and prediction (1217, 1242)
Journal
Geophysical Research Letters
http://www.agu.org/journals/gl/
Publisher
American Geophysical Union
2000 Florida Avenue N.W.
Washington, D.C. 20009-1277
USA
1-202-462-6900
1-202-328-0566
service@agu.org
Click to clear formClick to return to previous pageClick to submit