2-D Seismic Reflection Method Using Iso Velocity Method of Mianwali Area

Abstract

A seismic reflection of Line 12-B belonging to Mianwali Re-entrant was acquired and processed for 2-D interpretation. The line orients itself NNE-SSW direction. The sections have the shot points from VP-199 to VP-1044. Eleven Reflectors R1, R2, R3, Base Miocene, Pinchout P1, P2, P3, P4, P5P6 (Pinchout) are marked and a basement has been marked and interpreted. All the reflectors above the basement show a downward bending at the center. The depth of each reflector was calculated by iso velocity contour map method. The depth section obtained by this method shows stratigraphic features like Pinchouts. The reflectors are then correlated with the subsurface structures and stratigraphy of the area.

Share and Cite:

N. Khan, P. Zhu and S. Qureshi, "2-D Seismic Reflection Method Using Iso Velocity Method of Mianwali Area," International Journal of Geosciences, Vol. 4 No. 7, 2013, pp. 1073-1082. doi: 10.4236/ijg.2013.47101.

Conflicts of Interest

The authors declare no conflicts of interest.

References

[1] A. H. Kazmi and M. Q. Jan, “Geology and Tectonics of Pakistan,” Graphic Publishers, Karachi, 1997, 133p.
[2] A. N. Fatmi, M. Akthar, G. S. Alam and I. Hussain, “Geological Society of Salt Range,” Pakistan Geological Congress (GSP), Islamabad, 1984.
[3] M. P. Coward and R. W. H. Butler, “Thrust Tectonics and the Deep Structure of the Pakistan Himalaya,” Geology, Vol. 13, No. 6, 1985, pp. 247-265. doi:10.1130/0091-7613(1985)13<417:TTATDS>2.0.CO;2
[4] G. Sarwar and K. A. DeJong, “Arcs, Oroclines, Syntaxis: the Curvatures of Mountain Belts in Pakistan,” In: Geodynamics of Pakistan, Geological Survey of Pakistan, Quetta, 1979, pp. 342-349.
[5] R. S. Yeats and R. D. Lawrence, “Tectonics of the Himalayan Thrust Belt in northern Pakistan,” Marine Geology and Oceanography of Arabian Sea and Coastal Pakistan, Van Nostrand Reinhold Co., New York, 1984, pp. 177-200.
[6] A. Kemal, “Geology and New Trends for Hydrocarbon exploration in Pakistan,” Proceedings of International Petroleum Seminar, 22-24 November 1991, Islamabad, 1992, pp. 16-57.
[7] D. M. Baker, “Balanced Structural Cross Section of the Central Salt Range and Potwar Plateau of Pakistan— Shortening and over Thrust Deformation,” M.S. Thesis, Oregon State University, Corvallis, 1988, 120p.
[8] Kalabagh Consultants, III, “Geology and Geotechnical Assessment,” Project Planning Report, 1984, 12p.
[9] E. William, “Understanding the Effects of Structure and Bonding in the Bringelly Shale,” In: K. Alshibli, H. Malkawi and M. Alsaleh, Eds., Geo Jordan 2004: Advances in Geotechnical Engineering with Emphasis on Dams, Highway Materials, and Soil Improvement, American Society of Civil Engineers, Irbid, 2004, pp. 194-201.
[10] M. H. Malik and S. Farooq, “Geotechnical Aspects of the Dhoke Pathan Formation at the Kalabagh Dam Site,” The Geological Bulletin of the Punjab University, Vol. 23, 1998, pp. 117-127.
[11] O. Yilmaz, “Seismic Data Processing,” Society of Exploration Geophysicsts, Tulsa, 1987, 523p.
[12] H.-N. Al-Sadi, “Seismic Exploration Technique and Processing,” Birkhauser, Boston, 1980, 259p.
[13] L. Y. Faust, “Seismic Velocity as Function of Depth and Geologic Time,” Geophysics, Vol. 16, No. 2, 1951, pp. 206.
[14] E. S. Robinson and C. Coruh, “Basic Exploration Geophysics,” John Wiley & Sons, New York, 1988, 562p.
[15] M. B. Dobrin and C. H. Savit, “Introduction to Geophysical Prospecting,” 4th Edition, McGraw-Hill, New York, 1988, 867p.
[16] E. R. Gee, “Overview of Geology and Structure of Salt Range, with Observations on related Areas of Pakistan,” Geological Society of America, New York, 1980, pp. 28-232.

Copyright © 2024 by authors and Scientific Research Publishing Inc.

Creative Commons License

This work and the related PDF file are licensed under a Creative Commons Attribution 4.0 International License.