An airborne magnetometry study across Zagros collision zone along Ahvaz–Isfahan route in Iran

• Published in: Journal of applied geophysics 2015-12, Vol.123, p.112-122
• Main Authors: Oskooi, Behrooz, Abedi, Maysam
• Format: Article
• Language: English
• Subjects: Active fault; Airborne magnetic data; Geological zones; Magnetic data inversion; Stable downward continuation; Zagros
• ISSN: 0926-9851; 1879-1859
• DOI: 10.1016/j.jappgeo.2015.10.001

Convergence between the Eurasian and Arabian plates formed the Zagros orogenic belt between Late Cretaceous and Pliocene as a relatively young and active fold-thrust belt in Iran. The structural geology along Ahvaz to Isfahan route across Zagros is investigated employing magnetic data in order to determine the crustal structure in the collision zone of the two Palaeo-continents. Airborne magnetometry data with a line space of survey of 7.5km have been used to image the variations of the apparent magnetic susceptibility along this route. At first the airborne data were stably 500-m downward continued to the ground surface in order to enhance subtle changes of the Earth's magnetic field. Then 3D inverse modeling of magnetic data was implemented, while the cross section of the magnetic susceptibility variations along the route was mapped down to a depth of 100km. The acquired magnetic susceptibility model could appropriately predict the observed magnetic data as well. In addition, the analytic signal filter was applied to the reduced-to-pole magnetic data leading to the determination of active faults in Zagros fold-thrust belt (ZFTB) structural zone based upon the generated peaks. Some probable locations of fault events were also suggested in Sanandaj–Sirjan Zone (SSZ). The locations of faults correspond well to the magnetic susceptibility variations on the inverted section. Probable direction, slope and depth extension of these faults were also plotted on the magnetic susceptibility model, showing an intensively tectonized zone of the SSZ. The main difference between two domains is that the Eurasian plate seems to contain high magnetic susceptible materials compared to the Arabian plate. The recovered model of the apparent magnetic susceptibility values indicated that the average thickness of the non-magnetic sedimentary units is about 11km and the Curie depth locates approximately at depth of 24km for the whole studied area. [Display omitted] •The structural geology across Zagros is investigated employing magnetic data.•The magnetic susceptibility variations were mapped down to a depth of 100km.•The filtered magnetic data leading to determination of active faults in Zagros•The Eurasian plate contains high magnetic susceptible materials compared to the Arabian plate.