1887

Abstract

Following the strong earthquake occurred in the Abruzzo region (central Italy) on April 6, 2009 (Mw=6.3, Io=9 MCS), magnetotelluric (MT) and Deep Electrical Resistivity Tomography (DERT) have been carried out across the Aterno Valley, in the L’Aquila basin. The purpose of these different types of deep geophysical explorations has been to cast light on both the geometric relationships between the Quaternary deposits and the deeper mesocainozoic bedrock of the L’Aquila basin, and the electrical structure at seismogenic depth.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201401141
2010-06-14
2024-04-24
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201401141
Loading
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error