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Tectonics or magma intrusion?
-- new results from multi-parameter study
at Gede Volcano, West Java, Indonesia


D Hidayat1, H Gunawan2, M Hendrasto2, A Basuki2, F Schwandner1, S Marcial1, S
Kunrat2

1
  Earth Observatory of Singapore, Nanyang Technological University
2
 Center for Volcanology and Geological Hazard Mitigation, Indonesia
Gede Volcano,
West Java,
Indonesia

      JAKARTA




                                           Danau
  BOGOR                                   Jatiluhur




   Pangrango



      ©2009 Google – Map Data ©2009 and Europa Technologies
Eruptive history of Gede




Seismic behavior
at Gede
Monitoring Scheme          Initial no of station: 2 (1-component)
                           Currently: 9 stations (3 components:
For Gede & Salak Volcanoes BB and short period)
                                    Planned: 1 CO2 flux monitoring




                                        PUN
Example of data   Drumplot during normal period




                        Drumplot during swarm
Locatable VT at and around Gede Volcano May 2011– Aug 2012




                                              no report
Gede Hypocenters May 2011 – 26 Feb 2012
ede Hypocenters during swarm 27 Feb- 9 Apr 2012
Gede Hypocenters Aug 2012
Receiver function study reveals
2 low velocity zones under Gede
Gede Hypocenters during swarm vs Results from Receiver Function Study
Comparison with previous swarm




Hypocenters of 1997 swarm    Hypocenters of 2012 swarm
Tilt time-series




Deformation monitoring by
tiltmeters Jun-Jul 2011


                            Tilt vector
Tilt time-series




Deformation monitoring by
tiltmeters (Nov 2011-Feb 2012)


                                 Tilt vector 11/2011 – 26/02/2012
Tilt time-series




Deformation monitoring by
tiltmeters (27 Feb ’12-Jun ‘12)


                                  Tilt vector
Tilt time-series




Deformation monitoring by
tiltmeters (Aug-Sep 2012)




                            Tilt vector
Flank CO2 flux measurement campaigns
Highlight: 2011 NE sector: higher CO2 activity




                                                 2011-2012 flank CO2 flux :
                                                 •Campaigns:
                                                     • May, Sept 2011 (n 134)
                                                     • March 2012 (n 40)
                                                 •Method:
                                                     • high resolution CO2
                                                         accumulation chamber
                                                         (LICOR Li8100A)
                                                     • ~10 points/day, >3/site
                                                 •Results [CO2 g/m2/d]:
                                                     • 019.8 mean (2011)
                                                         112.5 max (2011)
                                                     • 011.7 mean (2012)
                                                         043.4 max (2012)
                                                 Compare flanks Gede -Merapi
                                                 mean ~40, max ~120 g/m2/day
                                                 (9/2002 at Woro)
                                                 Toutain et al. 2002, Figs.1,8
Possible source causing the earthquakes:

-tectonic related earthquakes (faulting)

-DVT (distal VT)
Concluding Remarks
-Prior to the swarm in Feb-Mar 2012 and Aug 2012, sequences of
small earthquakes occurred along NE-SW across Gede and
Pangrango.
-A short VT swarms occurred 27 Feb-8 Mar 2012. We postulates
that there may be a magma intrusion under Gede volcano but do
not lead to any eruption. Similar swarms occurred in 1997 were
located under Gede Volcano.
-Tilt data suggest deformation is controlled by local tectonic until
early Nov 2011. Then tilt vector change suggests inflation due to
(possibly) magma intrusion, followed by swarm of earthquakes at the
end of Feb 2012. Several months later tilt data is back to NE
direction. While CO2 flux measurements around Gede suggest some
high flux around NE from the volcano.
-Gede & Salak activity need to be continously monitored with multi-
parameter stations as any larger swarm, deformation, or gas flux
changes may lead to surface activity (eruption) which will affect
people living around the volcano.
Thank you

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Tectonics vs magma intrusion at Gede Volcano

  • 1. Tectonics or magma intrusion? -- new results from multi-parameter study at Gede Volcano, West Java, Indonesia D Hidayat1, H Gunawan2, M Hendrasto2, A Basuki2, F Schwandner1, S Marcial1, S Kunrat2 1 Earth Observatory of Singapore, Nanyang Technological University 2 Center for Volcanology and Geological Hazard Mitigation, Indonesia
  • 2. Gede Volcano, West Java, Indonesia JAKARTA Danau BOGOR Jatiluhur Pangrango ©2009 Google – Map Data ©2009 and Europa Technologies
  • 3. Eruptive history of Gede Seismic behavior at Gede
  • 4. Monitoring Scheme Initial no of station: 2 (1-component) Currently: 9 stations (3 components: For Gede & Salak Volcanoes BB and short period) Planned: 1 CO2 flux monitoring PUN
  • 5. Example of data Drumplot during normal period Drumplot during swarm
  • 6. Locatable VT at and around Gede Volcano May 2011– Aug 2012 no report
  • 7. Gede Hypocenters May 2011 – 26 Feb 2012
  • 8. ede Hypocenters during swarm 27 Feb- 9 Apr 2012
  • 10. Receiver function study reveals 2 low velocity zones under Gede
  • 11. Gede Hypocenters during swarm vs Results from Receiver Function Study
  • 12. Comparison with previous swarm Hypocenters of 1997 swarm Hypocenters of 2012 swarm
  • 13. Tilt time-series Deformation monitoring by tiltmeters Jun-Jul 2011 Tilt vector
  • 14. Tilt time-series Deformation monitoring by tiltmeters (Nov 2011-Feb 2012) Tilt vector 11/2011 – 26/02/2012
  • 15. Tilt time-series Deformation monitoring by tiltmeters (27 Feb ’12-Jun ‘12) Tilt vector
  • 16. Tilt time-series Deformation monitoring by tiltmeters (Aug-Sep 2012) Tilt vector
  • 17. Flank CO2 flux measurement campaigns Highlight: 2011 NE sector: higher CO2 activity 2011-2012 flank CO2 flux : •Campaigns: • May, Sept 2011 (n 134) • March 2012 (n 40) •Method: • high resolution CO2 accumulation chamber (LICOR Li8100A) • ~10 points/day, >3/site •Results [CO2 g/m2/d]: • 019.8 mean (2011) 112.5 max (2011) • 011.7 mean (2012) 043.4 max (2012) Compare flanks Gede -Merapi mean ~40, max ~120 g/m2/day (9/2002 at Woro) Toutain et al. 2002, Figs.1,8
  • 18. Possible source causing the earthquakes: -tectonic related earthquakes (faulting) -DVT (distal VT)
  • 19. Concluding Remarks -Prior to the swarm in Feb-Mar 2012 and Aug 2012, sequences of small earthquakes occurred along NE-SW across Gede and Pangrango. -A short VT swarms occurred 27 Feb-8 Mar 2012. We postulates that there may be a magma intrusion under Gede volcano but do not lead to any eruption. Similar swarms occurred in 1997 were located under Gede Volcano. -Tilt data suggest deformation is controlled by local tectonic until early Nov 2011. Then tilt vector change suggests inflation due to (possibly) magma intrusion, followed by swarm of earthquakes at the end of Feb 2012. Several months later tilt data is back to NE direction. While CO2 flux measurements around Gede suggest some high flux around NE from the volcano. -Gede & Salak activity need to be continously monitored with multi- parameter stations as any larger swarm, deformation, or gas flux changes may lead to surface activity (eruption) which will affect people living around the volcano.