The Use of Landsat 8 OLI Image for the Delineation of Gossanic Ridges in the Red Sea Hills of NE Sudan
[1]
Khalid A. Elsayed Zeinelabdein, Department of Geology, Faculty of Petroleum and Minerals, Al Neelain University, Khartoum, Sudan.
[2]
Abdel Halim H. El Nadi, Department of Geology, Faculty of Science, University of Khartoum, Khartoum, Sudan.
Gold mineralization type, associated with gossans, was discovered in Ariab area, through the analysis of Landsat images in the nineties of the last century. The main objective of this work is to delineate the gossanic ridges situated NW of Ariab area, which may represent prospective targets for gold mineralization. This can be achieved by applying the spectral band ratioing techniques on Landsat 8 OLI image. Application of the aforementioned techniques revealed characteristic signals of mineral alteration zones (gossanic ridges) that can be accurately mapped and verified by ground checks. XRF analysis of 12 chip samples collected randomly from the gossanic ridges confirmed the presence of gold in the area. Ore microscopic investigation of three samples of sheared gossans provided further evidence of gold mineralization in the study area. The present study demonstrated that the area is economically potential for gold owing to the large tonnage predicted from the delineated target zones.
Remote Sensing, Landsat 8, Gossans, Gold Mineralization, Red Sea Hills, Sudan
[1]
A.H. El Nadi and K.A. Elsayed Zeinelabdein. Geological report on the gold mineralization east of Wadi Gabgaba, northeastern Sudan. Unpub. report, 2011.
[2]
K.A. Elsayed Zeinelabdein. Sudan experience in using remote sensing for mineral prospecting. Proceedings of the 11th Arab International Conference on Mineral Resources, Arab Industrial Development and Mining Organization, Tripoli, Great Jamahiriya. p. 636-644, Oct. 25-27 2010.
[3]
W.R. Greenwood, D.G. Hadley, R.E. Anderson, R.J. Fleck and D.L. Schmidt. Late Proterozoic cratonization in southwestern Saudi Arabia. Phil. Trans. R. Soc. Lond. A, 280, 517-527, 1976.
[4]
I.G. Gass. The evolution of the Pan African crystalline basement in NE Africa and Arabia. J. Geol. Soc. Lond., 134, 129-138, 1977.
[5]
A. Kröner. Pan African plate tectonics and its reconstructions on the crust of north-east Africa. Geol. Rundsch. 68, 565-583, 1979.
[6]
A.H. El Nadi. The Geology of the Late Precambrian Meta-volcanics, Red Sea Hills, northeast Sudan. Ph.D. thesis, Nottingham University. 284 pp., 1984.
[7]
A.H. El Nadi. Late Precambrian volcanism in NE Sudan and the evolution of the Nubian Shield. Journal of the African Earth Sciences, Pergamon Press, London; Vol. 9, No. 3/4, 467-480, 1989.
[8]
D.C. Almond and F. Ahmed. Ductile shear zones in the northern Red Sea Hills, Sudan, and their implication for crustal collision. Geol. J., 22: 175-184, 1987.
[9]
A. Kröner, D. Linnebacher, R.J. Stern, T. Reichmann, Manton, and I.M. Hussein. Evolution of Pan African island arc assemblages in the southern Red Sea Hills, Sudan and southwestern Arabia as exemplified by geochemistry and geochronology. Precamb. Res. 53: 99-118, 1991.
[10]
D.B. Stoeser and J.S. Stacey. Evolution, U-Pb geochronology, and isotope geology of the Pan-African Nabitah orogenic belt of the Saudi Arabian Shield. In: The Pan-African belts of northeast Africa and Adjacent areas (Edited by El Gaby, S. and Greiling, R. O.) pp227- 288. Friedr Vieweg and Sohn, 1988.
[11]
M.G. Abdelsalam and R.J. Stern. Tectonic evolution of the Nakasib suture, Red Sea Hills, Sudan: evidence for a late Precambrian Wilson Cycle. J. Geol. Soc. London, Vol. 150: 393-404, 1993.
[12]
LDCM Landsat Data Continuity Mission. 29th Annual Louisiana RS/GIS Workshop. April 23, Cajundome Convention Center, Lafayette, Louisiana, 2013.
[13]
http://www.nasa.gov, accessed 25 June 2013.
[14]
Sabins, F.F. (1999). Remote sensing for mineral exploration. Ore Geology Reviews 14: 157–183.