NATIONAL AND KAPODISTRIAN UNIVERSITY OF ATHENS FACULTY OF GEOLOGY & GEOENVIRONMENT DEPARTMENT OF GEOPHYSICS & GEOTHERMICS Laboratory of Remote Sensing CRUSTAL DEFORMATION STUDIES IN THE SEISMICALLY ACTIVE AREA OF PATRAS GULF (GREECE)  Konstantina Vlachou,  Vassilis Sakkas,   Panagiotis Papadimitriou &  Evangelos Lagios
Aims of the Study Study the Regional and Local Ground Deformation Integrate DGPS & Seismological data to identify ground motion due to seismic activity and active tectonism Model major fault movements  Peloponnesus
Geodynamic Settings  Seismotectonic map of Greece
Main Geological Units
Seismic Activity 1980 - 2011 M>3.6 Mw=6.4 Mw=6.4 Mw=5.6 Mw=5.4 CTF Patras Gulf
The Patras Gulf GPS Network 10  Bench marks  1 Continuous GPS station (RLSO) – Established 2006 Campaigns  1994 1996  2006 2011
Rio – Antirrio Bridge  GPS network 7 Bench Marks 2008, 2009, 2011
DGPS Results 1994 – 2006 (ITRF 2000) Vertical Displacement
DGPS Results 1994 – 2006 Reference : No 50 Vertical Displacement 50
Strain Rate Field  Blue arrows: Extension Red arrows: Compression
Rio – Antirrio Bridge GPS net
Continuous GPS station RLSO  Station Velocit y  ( ETRF  )      Epoch 2005.00 CGPS  Station V East  (m m /yr) V North  (m m /yr) V Up  (m m /yr) RLSO -17.4 -15.2 +6.0 UoA1 -16.2 -22.4 +1.1 VLSM -6.4 -7.9 +0.5
(Mw=6.4,  June 8 th  2008) Andravida Earthquake
Mw=6.4 Time Series of RLSO station  2006 – present (ITRF 2000) Mw=6.4
Conclusions Opening up of the Patras Gulf at a rate of 8 – 13 mm/yr Uplift of the southern Part of  ≈ 5 mm/yr Westward increasing extension of the Patras Gulf  Smaller extension in the Rio – Antirrio Area ≈ 7 mm/yr RLSO CGPS station revealed SE horizontal motion with respect to ITRF2000  The 2008 Andravida Earthquake (Mw=6.4) was clearly depicted in RLSO CGPS station, with a northward offset of about 10 mm
“ Google Earth”  used to produce some of the Maps “ Generic Mapping Tool”  (GMT ) was used for all the figures “ Grid_Strain” s/w of  “Pesci A., Teza G., 2007” used for the strain calculation Acknowledgements  Thank you for your Attention !

Sakkas.ppt

  • 1.
    NATIONAL AND KAPODISTRIANUNIVERSITY OF ATHENS FACULTY OF GEOLOGY & GEOENVIRONMENT DEPARTMENT OF GEOPHYSICS & GEOTHERMICS Laboratory of Remote Sensing CRUSTAL DEFORMATION STUDIES IN THE SEISMICALLY ACTIVE AREA OF PATRAS GULF (GREECE) Konstantina Vlachou, Vassilis Sakkas, Panagiotis Papadimitriou & Evangelos Lagios
  • 2.
    Aims of theStudy Study the Regional and Local Ground Deformation Integrate DGPS & Seismological data to identify ground motion due to seismic activity and active tectonism Model major fault movements Peloponnesus
  • 3.
    Geodynamic Settings Seismotectonic map of Greece
  • 4.
  • 5.
    Seismic Activity 1980- 2011 M>3.6 Mw=6.4 Mw=6.4 Mw=5.6 Mw=5.4 CTF Patras Gulf
  • 6.
    The Patras GulfGPS Network 10 Bench marks 1 Continuous GPS station (RLSO) – Established 2006 Campaigns 1994 1996 2006 2011
  • 7.
    Rio – AntirrioBridge GPS network 7 Bench Marks 2008, 2009, 2011
  • 8.
    DGPS Results 1994– 2006 (ITRF 2000) Vertical Displacement
  • 9.
    DGPS Results 1994– 2006 Reference : No 50 Vertical Displacement 50
  • 10.
    Strain Rate Field Blue arrows: Extension Red arrows: Compression
  • 11.
    Rio – AntirrioBridge GPS net
  • 12.
    Continuous GPS stationRLSO Station Velocit y ( ETRF )    Epoch 2005.00 CGPS Station V East  (m m /yr) V North  (m m /yr) V Up  (m m /yr) RLSO -17.4 -15.2 +6.0 UoA1 -16.2 -22.4 +1.1 VLSM -6.4 -7.9 +0.5
  • 13.
    (Mw=6.4, June8 th 2008) Andravida Earthquake
  • 14.
    Mw=6.4 Time Seriesof RLSO station 2006 – present (ITRF 2000) Mw=6.4
  • 15.
    Conclusions Opening upof the Patras Gulf at a rate of 8 – 13 mm/yr Uplift of the southern Part of ≈ 5 mm/yr Westward increasing extension of the Patras Gulf Smaller extension in the Rio – Antirrio Area ≈ 7 mm/yr RLSO CGPS station revealed SE horizontal motion with respect to ITRF2000 The 2008 Andravida Earthquake (Mw=6.4) was clearly depicted in RLSO CGPS station, with a northward offset of about 10 mm
  • 16.
    “ Google Earth” used to produce some of the Maps “ Generic Mapping Tool” (GMT ) was used for all the figures “ Grid_Strain” s/w of “Pesci A., Teza G., 2007” used for the strain calculation Acknowledgements Thank you for your Attention !