• DocumentCode
    2809349
  • Title

    Application of Ground Penetrating Radar to detect orientation of cavities and caverns developed due to tectonic implication in Baratang Island, Middle Andaman, India

  • Author

    Ramanujam, N. ; Prasad, P. ; Vignesh, A. ; Murti, S.H.K. ; Rasool, Qazi Akhter ; Swapan, K.B. ; Ojha, Chandrakant ; Boopalan, A.J. ; Yuvaraj, P. Mothilal

  • Author_Institution
    Dept. of Coastal Disaster Manage., Pondicherry Univ., Pondicherry, India
  • fYear
    2012
  • fDate
    4-8 June 2012
  • Firstpage
    830
  • Lastpage
    834
  • Abstract
    Ground Penetrating Radar (GPR) is an effective tool to detect small (<; 10m diameter) caves and fissures in karst terrain. 170 caves have been identified within 1 km2 area in uplifted carbonate rocks in Baratang Island of Middle Andaman. Due to oblique subduction of Indian plate with Burmese plate in NW part of Andaman induced NE- SW and NW- SE trending sutures. The Study aims to validate the orientation of the fault patterns in carbonate rocks through Ground Penetrating Radar. To conduct GPR surveys two cave sites 400 m apart are selected. GPR - SIR-3000 instrument with dipole antenna in bistatic arrangement in reflection mode with stationary point mode is employed. Four depth (time) slices computed from the transect data for 40 MHz antenna with 500 ns range reflected across the cave No. 1 to a length of 19 m reveal bright linear features and intense spots positioned at the depths of 3 m and below 11 m to 18 m and vertical shaft connecting discontinuities are traced to 25 m depth in all plots. Five depth slices at an interval of 4.0 m to a total distance of 28 m with 40 MHz antenna with 400 ns have reflected bright regions at the depths from 8.5 m to 12.5 m and scanning up to depth of 20 m in cave No.2. Seven depth slices by using the 80 MHz antenna with time window of 250 ns across the cave No.2 have reflected to 12.5 m depth, show bright regions with high resolutions at the depth range of 8.5 to 12.5 m. Increase of antenna frequencies with lowering of time range has resolved high resolution reflections of cavities, cracks and reduction of depth in the cave No. 2 than the in cave No. 1. Induction of cracks and fissures in carbonate rocks due to erstwhile tectonic repercussion were subsequently increased their sizes through rain water percolation and dissolution. Depth (time) slices of GPR in all transects across the cave orientations in two sites proved that continuation of caves are aligned in NW-SE and NE-SW directions.
  • Keywords
    faulting; geophysical equipment; ground penetrating radar; remote sensing by radar; rocks; Baratang Island; Burmese plate; GPR-SIR-3000 instrument; Indian plate; bistatic dipole antenna; carbonate rock cracks; carbonate rock fissures; cavern orientation detection; cavity orientation detection; depth 3 m to 25 m; distance 28 m; fault pattern orientation; frequency 40 MHz; frequency 80 MHz; ground penetrating radar; karst terrain; middle Andaman; oblique tectonic plate subduction; rain water dissolution; rain water percolation; reflection mode operation; size 19 m; stationary point mode; tectonic implication; time 250 ns; time 400 ns; time 500 ns; uplifted carbonate rocks; Cavity resonators; Ground penetrating radar; Radar antennas; Reflection; Reflector antennas; Rocks; Andaman; Ground penetrating radar; calcareous sandstone; cavern;
  • fLanguage
    English
  • Publisher
    ieee
  • Conference_Titel
    Ground Penetrating Radar (GPR), 2012 14th International Conference on
  • Conference_Location
    Shanghai
  • Print_ISBN
    978-1-4673-2662-9
  • Type

    conf

  • DOI
    10.1109/ICGPR.2012.6254977
  • Filename
    6254977