Abstract
The heavy mineralogical investigation of the soil sample involved from the Khurrianuiala soil series suggests a mixed parentage dominated by schists of low, e.g., chlorite to high, e.g., hyanite, c.rade together with: mafic igneous, e.g., clinopyroxene. lnuestigations of the quartz grains at submicroscopic level revealed the solution and precipitation of Si02 .nH2 0, alongwith V-shaped etching as the main shaping mechanisms of minerals.

DA Jenkins, R.H.Qureshi. (1990) EAVY MINERALS SEPARATION AND THEIR STUDY BY TH, , Volume 27, Issue 4.
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