Lithogeochemical Prospecting Through Stream Sediments in Bela Ophiolite of Lasbela Area
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) KAU : En" " Sci., vol. 7, pp. 125-142 (1414 A .H. /1994 A .D .) Lithogeochemical Prospecting Through Stream Sediments in Bela Ophiolite of Lasbela Area SHAHID NASEEM and SHAMIM AHMED SHEIKH Department of Geology, University of Karachi, Karachi, Pakistan ABSTRACT. Lithogeochemical investigation of sediments of active streams draining through Bela Ophiolite, from Lasbela area are presented . This area consists mainly of ophiolites associated with sedimentary rocks of Jurassic-Cretaceous age. Quantitative examinations of important immobile ·elements such as Fe, Mn, Ti & Cr, and semi-mobile to mobile like Zn , Cu, Ni and Co have been carried out , These elements have anomalous concern - rations in fine stream sediments in certain regions. An attempt is made to demarcate the areas of possible occurrences of ore mineralization as- sociated with the Bela Oph iolite based on statistical analysis of the geochemical data. .Statistical analysis and plots of data were employed to evaluate the dis- tribution and interrelationship of these clements and coefficient of varia- tion and correlation coefficients were calculated. The suitability of the methods is discussed in relation with the arid climaticconditions of southern Balochistan and the local geology. Introduction Methods of prospecting for mineral and ore deposits through stream sediments using lithogeochemical techniques are being successfully employed in different parts of the world. Sampattavanija (1963), Bloomfield et al. (1971), Beeson (1984) and Hashimi (1986) have studied and used stream sediments for prospecting. Wahid (1%3), Sid- diqi (1976) and Bozdar (1982) emphasized the application of geochemical prospect- ing methods in Pakistan to exploit esoteric mineral deposits. Stream sediments are derived from the weathering of rocks and are dispersed in stream channels. Commonly, the stream sediments include unaltered primary min- 125
Transcript of Lithogeochemical Prospecting Through Stream Sediments in Bela Ophiolite of Lasbela Area
) KAU : En" " Sci., vol. 7, pp. 125-142 (1414 A .H. /1994 A .D .)
Lithogeochemical Prospecting Through Stream Sedimentsin Bela Ophiolite of Lasbela Area
SHAHID NASEEM and SHAMIM AHMED SHEIKHDepartment of Geology, University of Karachi,
Karachi, Pakistan
ABSTRACT. Lithogeochemical investigation of sediments of active streamsdraining through Bela Ophiolite, from Lasbela area are presented . Thisarea consists mainly of ophiolites associated with sedimentary rocks ofJurassic-Cretaceous age . Quantitative examinations of important immobile·e lements such as Fe, Mn, Ti & Cr, and semi-mobile to mobile like Zn , Cu,Ni and Co have been carried out , These elements have anomalous concern rations in fine stream sediments in certain regions . An attempt is made todemarcate the areas of possible occurrences of ore mineralization associated with the Bela Ophiolite based on statistical analysis of thegeochemical data.
. Statistical analysis and plots of data were employed to evaluate the distribution and interrelationship of these clements and coefficient of variation and correlation coefficients were calculated. The suitability of themethods is discussed in relation with the arid climatic conditions ofsouthernBalochistan and the local geology .
Introduction
Methods of prospecting for mineral and ore deposits through stream sediments usinglithogeochemical techniques are being successfully employed in different parts of theworld. Sampattavanija (1963), Bloomfield et al. (1971), Beeson (1984) and Hashimi(1986) have studied and used stream sediments for prospecting. Wahid (1%3), Siddiqi (1976) and Bozdar (1982) emphasized the application of geochemical prospecting methods in Pakistan to exploit esoteric mineral deposits.
Stream sediments are derived from the weathering of rocks and are dispersed instream channels. Commonly, the stream sediments include unaltered primary min-
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