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@ARTICLE{Bechtold:4868,
      author       = {Bechtold, M. and Battaglia, M. and Tanner, D. C. and
                      Zuliani, D.},
      title        = {{C}onstraints on the active tectonics of the {F}riuli/{NW}
                      {S}lovenia area from {CGPS} measurements and
                      three-dimensional kinematic modeling},
      journal      = {Journal of geophysical research / Atmospheres},
      volume       = {114},
      issn         = {0148-0227},
      address      = {Washington, DC},
      publisher    = {Union},
      reportid     = {PreJuSER-4868},
      year         = {2009},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {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.},
      keywords     = {J (WoSType)},
      cin          = {ICG-4},
      ddc          = {550},
      cid          = {I:(DE-Juel1)VDB793},
      pnm          = {Terrestrische Umwelt},
      pid          = {G:(DE-Juel1)FUEK407},
      shelfmark    = {Geochemistry $\&$ Geophysics},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000264686700001},
      doi          = {10.1029/2008JB005638.},
      url          = {https://juser.fz-juelich.de/record/4868},
}