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| Home > Publications database > Constraints on the active tectonics of the Friuli/NW Slovenia area from CGPS measurements and three-dimensional kinematic modeling > print |
| 001 | 4868 | ||
| 005 | 20200423202517.0 | ||
| 024 | 7 | _ | |a 10.1029/2008JB005638. |2 DOI |
| 024 | 7 | _ | |a WOS:000264686700001 |2 WOS |
| 024 | 7 | _ | |a 0141-8637 |2 ISSN |
| 024 | 7 | _ | |a 2128/20444 |2 Handle |
| 037 | _ | _ | |a PreJuSER-4868 |
| 041 | _ | _ | |a eng |
| 082 | _ | _ | |a 550 |
| 084 | _ | _ | |2 WoS |a Geochemistry & Geophysics |
| 100 | 1 | _ | |a Bechtold, M. |b 0 |u FZJ |0 P:(DE-Juel1)129436 |
| 245 | _ | _ | |a Constraints on the active tectonics of the Friuli/NW Slovenia area from CGPS measurements and three-dimensional kinematic modeling |
| 260 | _ | _ | |c 2009 |a Washington, DC |b Union |
| 300 | _ | _ | |a |
| 336 | 7 | _ | |a Journal Article |0 PUB:(DE-HGF)16 |2 PUB:(DE-HGF) |
| 336 | 7 | _ | |a Output Types/Journal article |2 DataCite |
| 336 | 7 | _ | |a Journal Article |0 0 |2 EndNote |
| 336 | 7 | _ | |a ARTICLE |2 BibTeX |
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| 336 | 7 | _ | |a article |2 DRIVER |
| 440 | _ | 0 | |a Journal of Geophysical Research-Solid Earth |x 0148-0227 |0 20882 |v 114 |
| 500 | _ | _ | |a Record converted from VDB: 12.11.2012 |
| 520 | _ | _ | |a We use site velocities from continuous GPS (CGPS) observations and kinematic modeling to investigate the active tectonics of the Friuli/NW Slovenia area. Data from 42 CGPS stations around the Adriatic indicate an oblique collision, with southern Friuli moving NNW toward northern Friuli at the relative speed of 1.6 to 2.2 mm/a. We investigate the active tectonics using 3DMove, a three-dimensional kinematic model tool. The model consists of one indenter-shaped fault plane that approximates the Adriatic plate boundary. Using the "fault-parallel flow'' deformation algorithm, we move the hanging wall along the fault plane in the direction indicated by the GPS velocities. The resulting strain field is used for structural interpretation. We identify a pattern of coincident strain maxima and high vorticity that correlates well with groups of hypocenters of major earthquakes (including their aftershocks) and indicates the orientation of secondary, active faults. The pattern reveals structures both parallel and perpendicular to the strike of the primary fault. In the eastern sector, which shows more complex tectonics, these two sets of faults probably form an interacting strike-slip system. |
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| 650 | _ | 7 | |a J |2 WoSType |
| 653 | 2 | 0 | |2 Author |a Friuli |
| 653 | 2 | 0 | |2 Author |a deformation velocities |
| 653 | 2 | 0 | |2 Author |a strain field |
| 653 | 2 | 0 | |2 Author |a tectonics |
| 700 | 1 | _ | |a Battaglia, M. |b 1 |0 P:(DE-HGF)0 |
| 700 | 1 | _ | |a Tanner, D. C. |b 2 |0 P:(DE-HGF)0 |
| 700 | 1 | _ | |a Zuliani, D. |b 3 |0 P:(DE-HGF)0 |
| 773 | _ | _ | |0 PERI:(DE-600)2016800-7 |a 10.1029/2008JB005638. |g Vol. 114 |q 114 |v 114 |x 0148-0227 |y 2009 |t Journal of geophysical research / Atmospheres |
| 856 | 7 | _ | |u http://dx.doi.org/10.1029/2008JB005638. |
| 856 | 4 | _ | |u https://juser.fz-juelich.de/record/4868/files/2008JB005638.pdf |y OpenAccess |
| 856 | 4 | _ | |u https://juser.fz-juelich.de/record/4868/files/2008JB005638.pdf?subformat=pdfa |x pdfa |y OpenAccess |
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| 914 | 1 | _ | |y 2009 |
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