Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
9526998 | Tectonophysics | 2005 | 22 Pages |
Abstract
Based on the 2-D seismic velocity model, a density model is developed. Density values are assigned to each layer in agreement with the P-wave velocity model and with values accepted for the geological units in the area. After several iterations a good fit between the computed and observed Bouguer anomalies was obtained along the seismic line.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
V. Raileanu, A. Bala, F. Hauser, C. Prodehl, W. Fielitz,