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Abstract:The southern part of Kadiri Schist Belt is in juxtaposition with granitoids on either side which include TTG, TGM, and MS suites. The schist belt rocks and granitoids exhibit three phases of deformation. The granitoids are mainly medium to coarse grained and exhibit hypidiomorphic texture. Geochemical signatures suggest that the granitoids are magmatic, metaluminous, calc-alkaline and grouped under mixed origin. The field, mineralogical and chemical observations discriminate them as I-type. Petrogenetic studies indicate that polyphase polymigmatised TTG gneisses show the existence of older simatic crust which later gave rise to varied sialic crust in marginal basin environment. The calc-alkaline TGM suite points to magma mingling and mixing and fractional crystallization differentiation. The MS suite has evolved due to crustal anatexis and mantle derived melts.
Keywords : Granitoids, Kadiri Schist Belt, Magma mingling and mixing, Petrology.
pp.1-12.
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Abstract:The performance of drilling bits has a direct influence on cost and increase in the rate of penetration translates significantly to cost and time saving. From a total sample of 56 wells, approximately 450 tri-cone bits were consumed at a cost of KSh 200Millions.
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Keywords: Domestic water sources, physico-chemical properties, water quality, Atomic Absorption Spectrometry (AAS), heavy metal concentration.
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