Memoirs of the Geological Survey of Pakistan, Volume 15The Survey, 1985 |
From inside the book
Results 1-3 of 14
Page 5
... probably Nari / Gaj in the Thano Bula Khan area . About 5 to 10 km . north of Thano Bula Khan , along the Karchat road some wells are producing water from a sandstone unit from depths of 6 to 15 m but the water is very brackish . A tube ...
... probably Nari / Gaj in the Thano Bula Khan area . About 5 to 10 km . north of Thano Bula Khan , along the Karchat road some wells are producing water from a sandstone unit from depths of 6 to 15 m but the water is very brackish . A tube ...
Page 3-11
... probably created undulation as observed in the resistiv- ity curve Similarly in the other two areas the consistant trends of the aquifers indicate that the aquifers are controlled by the uniform geologic structures which holds true for ...
... probably created undulation as observed in the resistiv- ity curve Similarly in the other two areas the consistant trends of the aquifers indicate that the aquifers are controlled by the uniform geologic structures which holds true for ...
Page 4-10
... probably due to a fault ( Amin Khan & R.A. Khan , 1976 , 1983 ) . The effluent characteristic of the naddi proba- bly changes as the water disappears under ground since the area thereaf- ter is identified as saline water zone . The ...
... probably due to a fault ( Amin Khan & R.A. Khan , 1976 , 1983 ) . The effluent characteristic of the naddi proba- bly changes as the water disappears under ground since the area thereaf- ter is identified as saline water zone . The ...
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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