Impact of the 6 April 2009 L'Aquila earthquake on groundwater flow in the Gran Sasso carbonate aquifer, Central Italy
- 28 December 2010
- journal article
- research article
- Published by Wiley in Hydrological Processes
- Vol. 25 (11), 1754-1764
- https://doi.org/10.1002/hyp.7933
Abstract
No abstract availableThis publication has 35 references indexed in Scilit:
- Limits on earthquake nucleation and other pre‐seismic phenomena from continuous strain in the near field of the 2009 L'Aquila earthquakeGeophysical Research Letters, 2010
- Rupture history of the 2009 L'Aquila (Italy) earthquake from non‐linear joint inversion of strong motion and GPS dataGeophysical Research Letters, 2009
- The 2009 L'Aquila (central Italy) MW6.3 earthquake: Main shock and aftershocksGeophysical Research Letters, 2009
- Coseismic deformation of the destructive April 6, 2009 L'Aquila earthquake (central Italy) from GPS dataGeophysical Research Letters, 2009
- Chemical and isotopic (δ18O‰, δ2H‰, δ13C‰, 222Rn) multi-tracing for groundwater conceptual model of carbonate aquifer (Gran Sasso INFN underground laboratory – central Italy)Journal of Hydrology, 2008
- Stable isotope (2H, 18O and 87Sr/86Sr) and hydrochemistry monitoring for groundwater hydrodynamics analysis in a karst aquifer (Gran Sasso, Central Italy)Applied Geochemistry, 2005
- Carbon 13 of TDIC to quantify the role of the unsaturated zone: the example of the Vaucluse karst systems (Southeastern France)Journal of Hydrology, 2003
- Origin of postseismic streamflow changes inferred from baseflow recession and magnitude‐distance relationsGeophysical Research Letters, 2001
- New empirical relationships between magnitude and distance for liquefactionTectonophysics, 2000
- In search of earthquake-related hydrologic and chemical changes along Hayward FaultApplied Geochemistry, 1994