| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9526987 | Tectonophysics | 2005 | 20 Pages |
Abstract
The different sub-recent stress fields and related fault patterns might succeed each other or might alternate through time. The first and third deformations have fresh topographic expressions and cannot play synchronously. The observed features suggest a compressionally active neotectonics of the study area.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Á. Magyari, B. Musitz, L. Csontos, B. Van Vliet-Lanoë,