University of Tehran Press Journal of the Earth and Space Physics 2538-371X 27 1 2001 03 21 - - 13323 FA Journal Article 1970 01 01 This paper describes a methodology for the integrated interpretation of airborne magnetic and airborne y-ray spectrometer data. The Darrehzar porphyry copper deposit is situated in the Uromieh-Dokhtar magmatic assemblage of Central Iran. Phyllic and propylitic alteration are pervasive in the area but potassic and argillic alterations are not readily recognized on the surface. The spatial distributions of geophysical data resemble the lithological and alteration patterns in the area. The Darrehzar porphyry copper deposit is considered as a control site for determination of the degree that the geophysical data is correlated with the mineralization zone. Airborne magnetic/radiometric, geochemical /alteration and ground geophysical data sets have been integrated and analyzed using canonical correlation method. This technique is found to be useful for the delineation of hydrothermally altered areas and data compression. This paper describes a methodology for the integrated interpretation of airborne magnetic and airborne y-ray spectrometer data. The Darrehzar porphyry copper deposit is situated in the Uromieh-Dokhtar magmatic assemblage of Central Iran. Phyllic and propylitic alteration are pervasive in the area but potassic and argillic alterations are not readily recognized on the surface. The spatial distributions of geophysical data resemble the lithological and alteration patterns in the area. The Darrehzar porphyry copper deposit is considered as a control site for determination of the degree that the geophysical data is correlated with the mineralization zone. Airborne magnetic/radiometric, geochemical /alteration and ground geophysical data sets have been integrated and analyzed using canonical correlation method. This technique is found to be useful for the delineation of hydrothermally altered areas and data compression. https://jesphys.ut.ac.ir/article_13323_2ac05eeb337b40a140bfb98e13dc1eaf.pdf