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A Comparison of SED, Special Functions and Euler Deconvolution to Identify Magnetic Lineaments in Khuzestan PlainNormal access

Authors: Z. Mahmoodpour, F. Molaei and H. Siavoshi
Event name: 2nd Conference on Geophysics for Mineral Exploration and Mining
Session: Application of Airborne Geophysical Methods for Depth-to-Basement and Sediment Cover Imaging
Publication date: 09 September 2018
DOI: 10.3997/2214-4609.201802721
Organisations: EAGE
Language: English
Info: Extended abstract, PDF ( 3.13Mb )
Price: € 20

Summary:
Geological structures are not often cylindrical and can result from complex deformation histories. Lineament is one of the complex structures on the land surface. It is a linear feature in a landscape that is an expression of an underlying geological structure such as a fault. Typically, a lineament is comprised of a fault-aligned valley, a series of fault or fold-aligned hills, a straight coastline or a combination of these features. Fracture zones, shear zones and igneous intrusions such as dykes can also give rise to lineaments. Lineaments are often apparent in geological or topographic maps and can appear on aerial or satellite photographs or aeromagnetic maps.


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