The use of geomagnetic for
geophysical and geological studies is a new method for receiving different
information from new and old faults and lineaments. Accordingly, the present
study is applied research and it use combined the two methods, analytical
signal and Euler’s combined method and invented a new combined method to
estimate the depth, location and shape of the magnetic and gravity sources. As
a case, this research selected Iran’s Zagros zone. This region due to the
geological dynamics is considered by many geologists. In this regard, the
1:250,000 framework of Haji Abad was selected as a case study because of its
convenient location for structural analysis. As a result, with airborne
magnetic images survey, and applying filters in the vertical derivative and
analytical signal, lineaments in depth of this region discovered and
investigated.
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http://dx.doi.org/10.1029/RF003p0189
http://wellog.com/RF003p0189.pdf
[10]
McEnroe, S.A., Robinson, P., Langenhorst, F., Frandsen, C., Terry, M.P. and Boffa Ballaran, T. (2007) Magnetization of Exsolution Intergrowths of Hematite and Ilmenite: Mineral Chemistry, Phase Relations, and Magnetic Properties of Hemo-Ilmenite Ores with Micron—to Nanometer—Scale lamellae from Allard Lake, Quebec. Journal of Geophysical Research: Solid Earth (1978-2012), 112. http://onlinelibrary.wiley.com/doi/10.1029/2007JB004973/full
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Salem, A. and Ravat, D. (2003) A Combined Analytic Signal and Euler Method (AN-EUL) for Automatic Interpretation of Magnetic Data. Geophysics, 68, 1952-1961. http://dx.doi.org/10.1190/1.1635049
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Gregory, A.W. and Hansen, B.E. (1996) Residual-Based Tests for Cointegration in Models with Regime Shifts. Journal of Econometrics, 70, 99-126. http://dx.doi.org/10.1016/0304-4076(69)41685-7
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