Behavior of seismic wave propagation with respect to fracture orientations in limestone, Perak, Malaysia

  • Authors

    • Eko March Handoko Bin Masyhur
    • Abdul Ghani Abd Rafek
    • Khairul Arifin Mohd Noh
    2018-11-30
    https://doi.org/10.14419/ijet.v7i4.28.22620

  • Abstract

    Conventional shallow surface seismic refraction survey is associated with long elastic wavelength thus it is often ignoring the existence of cracks and fractures underneath.  Fracture has essential effect on reducing seismic velocity.  This paper highlights the velocity variation in different direction with respect to preferred orientation of fracture sets of limestone in a quarry located at Chemor, Perak, Malaysia.  Multi azimuth seismic refraction survey in the orientation of fan shooting is utilized to records seismic velocity from different azimuth.  Slowness concept is used to study the responses of seismic wave velocity in regards to the discontinuity orientation.  The analysis of the results indicate seismic wave propagates faster in the direction parallel with the strike of the fracture.  The seismic wave experience largest time delay as the wave propagates perpendicular with the strike direction of the fracture structure.  With this behavior of seismic wave in respect to the fractures orientation, it is possible to map the extension of the orientation of subsurface fractures.

  • References

    1. [1] Khoo, T T, and B K Tan. 1983. “Geological Evolution of Peninsular Malaysia.†Workshop on Stratigraphic Correlation of Thailand and Malaysia: 253–90.

      [2] Kleczek, Iwona Stan, and Adam F Idziak. 2008. “Anisotropy of Elastic Properties of Rock Mass Induced by Cracks.†Acta Geodyn. Geomater 5(2): 153–59.

      [3] Masuda, H. 1964. “Utilisation of Elastic Longitudinal Wave Velocity for Determining the Elastic Property of Dam Foundation Rocks.†International Congress on Large Dams, 1(Q28): 253–69.

      [4] Nassir Saeed, Abdul, Abdul Ghani Rafek, Rahman Yaccup, and Abdul Rahim Samsudin. 2000. “Application of P & SH-Waves for Rock Anisotropy Studies: Genting Highlands Case Study.†Geological Society of Malaysia Bulletin 44(July): 69–73.

      [5] Nur, Amos, and Gene Simmons. 1969. “Stress-Induced Velocity Anisotropy in Rock: An Experimental Study.†Journal of Geophysical Research 74(27): 6667.

      [6] Oberti, G., E. Carabelli, L. Goffi, and P.P Rossi. 1979. “Study of an Orthotropic Rock Mass: Experimental Techniques, Comparative Analysis of Results.†Proceeding of 4th Congress Rock Mechanics (ISRM), Montreux 2: 485–91.

      [7] Palmer, Derceke. 1981. “An Introduction to the Generalized Reciprocal Method of Seismic Refraction Interpretation.†GEOPHYSICS 46(11): 1508–18.

      [8] Rafek, Abdul Ghani. 1985. “Penentuan Kualitatif Anisotropi Jasad Batuan Dengan Menggunakan Kaedah Biasan Seismik.†Sains Malaysiana 1(14): 153–72.

      [9] Stan, Iwona, and Adam F Idziak. 2005. “Anisotropy of Seismic Waves Velocity Due to the Fracturing in Chosen Rock Mass.†Eurock 2005 - Impact of Human Activity on the Geological Environment: 579–86.

  • Downloads

  • How to Cite

    Masyhur, E. M. H. B., Rafek, A. G. A., & Noh, K. A. M. (2018). Behavior of seismic wave propagation with respect to fracture orientations in limestone, Perak, Malaysia. International Journal of Engineering & Technology, 7(4.28), 400-403. https://doi.org/10.14419/ijet.v7i4.28.22620

    Received date: 2018-11-30

    Accepted date: 2018-11-30

    Published date: 2018-11-30