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International Journal of Geography and Geology

February 2015, Volume 4, 2, pp 37-46

Investigating the Density Ratios of Geological Structure through Fractal Geometry Case Stady: (Dehno Region in Farss of Iran)

Shadi Asoodeh


Asghar Teymoorian Motlagh

Shadi Asoodeh 1

Asghar Teymoorian Motlagh 2

  1. M.Sc. degree on Geophysics, Hamedan Branch, Islamic Azad University, Hamedan, Iran 1

  2. Departments of Geophysics, Hamedan Branch, Islamic Azad University, Hamedan, Iran 2

Pages: 37-46

DOI: 10.18488/journal.10/2015.4.2/

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One of the most important steps to obtain the specified density Bouguer anomaly corrections for the topography of the page Bouguer is the most commonly used way in which the relationship between topography and Bouguer anomaly in the method assumes that topography of the rigid shell instead Isostasy balance is maintained. The method to determine the density of Bouguer provided by fractal analyze these are the lowest density dependence the topography of the area is considered as the optimal density and the fractal relationship to the topography of the fractal dimension using the Bouguer anomaly. 

Contribution/ Originality




  1. Aronson, P.B. and D.M.S. Mark, 1984. Scale-depandent fractal, dirmehsion of topographic surfaces. Math. Ged., 16(5): 671-683.
  2. Genevraye, P., M. Seguret, S. Nikpour, C. Moulle, R. Perrier and P. Ahmadnia, 1967. Dehno and namaki geological survey, total Iran petroleum co. Report No. 5517-9-1.
  3. Hasaani Pak, A., 2004. Exploratory data analysis. Tehran University Press.
  4. Kavoosi, M., 2000. Stratigraphy and sedimentology of tertiary deposits in fars sedimentary basin. Geology Report of the National Iranian Oil Company.
  5. Nettleton, L., 1939. Determinetion of density for reduction of gravimeter observations. Geophysics, 4(3).
  6. Telford, M., 2008. Applied geophysics. Trans. by Dr. HosseinHajeb-Hoseinieh. Tehran University Press.
  7. Thorrarinsson, F. and S.G. Magnusson, 1990. Bouguer density determination by fractal analysis. Geophysics, 3(2).


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