Memoirs of the Geological Survey of Pakistan, Volume 15The Survey, 1985 |
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... encountered at deeper levels in northern parts of the basin and at shallower levels in the south , suggesting a control of flow of groundwater from topo- structural high in the north to topostructural low areas in the south . b2 ...
... encountered at deeper levels in northern parts of the basin and at shallower levels in the south , suggesting a control of flow of groundwater from topo- structural high in the north to topostructural low areas in the south . b2 ...
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... encountered and confirmed the sandstone units upto drill depth of 148m . ( see table 2 ) . More aqui- fers at depth greater than 148m . are likely to be encountered . nificant . The potential of Nari Formation aquifers is expected to be ...
... encountered and confirmed the sandstone units upto drill depth of 148m . ( see table 2 ) . More aqui- fers at depth greater than 148m . are likely to be encountered . nificant . The potential of Nari Formation aquifers is expected to be ...
Page 12
... encountered in drill holes in various and final interpretation is given in Table 2 ) . Aquifers in Unconsolidated Sediments ma- From the comparative statement it can be seen that good development of unconsolidated material is not ...
... encountered in drill holes in various and final interpretation is given in Table 2 ) . Aquifers in Unconsolidated Sediments ma- From the comparative statement it can be seen that good development of unconsolidated material is not ...
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Common terms and phrases
alluvium aquifers average Band Baran brackish clay colour consolidated correlation cover curves deposits depth diameter discharge District Drill Hole drilling feet field flow Gadap basin Gaj Formation Geological Goth grained gravel gray ground water groundwater hour inches indicated inferred interpretation Kalu Khuhar Karchat Valleys Khadeji layers less limestone limited lithology located Malir basin Manchar Formation material medium meters mixed MONTHLY Nadi Nari Formation observed ohm cms Pakistan places Pleistocene potential present probably probe pumping test quality of water rainfall ranges reference region resistivity resistivity measurements resistivity ranges Resources Results river rock saline salt sand sandstone saturated sediments shallow SHOWING silt stone stream surface Survey synclinal Table test hole Thano Bula Khan thickness thin unconsolidated units Upper Malir valley values VARIATION varies zone اور کی کے میں ہے