1887

Abstract

The study of spatial characteristics of seismic attenuation has been performed in the NW part of Dobrogea, between Trotus fault and Peceneaga – Camena fault, on the boundary between East-European and Moesian tectonic plates. This study is based on a number of 105 recordings of the K2 network, using the recordings derived from 16 seismic events generated in the range 3 - 20 km. An estimation of the attenuation factor Q was made in the mentioned area, obtaining a value of 488 for the crust.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.20145550
2010-05-04
2021-01-28
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20145550
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