The Mw D 6Ð3 L'Aquila earthquake on 6 April 2009 produced a mainshock that caused significant changes in the hydrogeology of the Gran Sasso carbonate fractured aquifer: (i) the sudden disappearance at the time of the mainshock of some springs located exactly along the surface trace of the Paganica n
Headache prevalence in the population of L’Aquila (Italy) after the 2009 earthquake
✍ Scribed by Cristiana Guetti; Chiara Angeletti; Roberta Papola; Emiliano Petrucci; Maria Laura Ursini; Alessandra Ciccozzi; Franco Marinangeli; Antonella Paladini; Giustino Varrassi
- Publisher
- Springer
- Year
- 2011
- Tongue
- English
- Weight
- 200 KB
- Volume
- 12
- Category
- Article
- ISSN
- 1129-2369
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On 6 April 2009, 01:32 GMT, an M w 6.3 earthquake hit the Abruzzi region of central Italy causing widespread damage in the City of L'Aquila and its nearby villages. The mainshock of this earthquake was recorded by 57 digital strong-motion instruments, four of which are located on the hanging wall of
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