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

Authors

  • Shadi Asoodeh M.Sc. degree on Geophysics, Hamedan Branch, Islamic Azad University, Hamedan, Iran
  • Asghar Teymoorian Motlagh Departments of Geophysics, Hamedan Branch, Islamic Azad University, Hamedan, Iran

DOI:

https://doi.org/10.18488/journal.10/2015.4.2/10.2.37.46

Abstract

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.

Keywords:

Fractal dimension, Topography, Bouguer anomaly, Optimal density, Isostasy, Dehno region

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Published

2015-01-15

How to Cite

Asoodeh, S. ., & Motlagh, A. T. . (2015). Investigating the Density Ratios of Geological Structure through Fractal Geometry Case Stady: (Dehno Region in Farss of Iran). International Journal of Geography and Geology, 4(2), 37–46. https://doi.org/10.18488/journal.10/2015.4.2/10.2.37.46

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