2016
DOI: 10.3329/jbcps.v33i2.28046
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Detection of Omental Recurrence of Colorectal Cancer by FDG-PET/CT

Abstract: not availableJ Bangladesh Coll Phys Surg 2015; 33(2): 105-106

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“…vertical displacements A NW-SE trending major fault marking the northern limit of the basin A N –S trending bounding fault marking the eastern limit of the basin Groundwater layer in the vicinity No aquifer in the vicinity; safer distance (∼600 m ) from overlying Dupi Tila aquifer. Active aquifer is unconformably overlying Minor groundwater source in the vicinity; 2nd aquifer with lower hydraulic conductivity Coal beds are overlain by Dupi Tila aquifer, major GW source Regional aquifer Dupi Tila on top Overburden/Roof materials (preferably Impervious) 150–200 m cover of hard, compacted, impervious Gondwana sandstone 140 m thick Permian Gondwana sandstone (aquifer) in hydraulic continuity with the seam VI 184 m Gy mudstone, sandstone and pebble interbeds of Surma group, lower permeability >300 m of poorly consolidated water- bearing sandy layer forming Dupi Tila aquifer unconformably overlain by loosely consolidated Upper Tertiary Dupi Tila sandy formation Hydraulic head 108 bar Seam dipping 5°–15° 12° (seam VI) 13.4° (seam-II) Reserve (Million Ton) 1053 390 685 865 572 Cited [ 1 , [83] , [84] , [85] ] [ 73 , 86 ] [ 72 , 87 ] [ 75 , 88 ] [ …”
Section: Methodsmentioning
confidence: 99%
“…vertical displacements A NW-SE trending major fault marking the northern limit of the basin A N –S trending bounding fault marking the eastern limit of the basin Groundwater layer in the vicinity No aquifer in the vicinity; safer distance (∼600 m ) from overlying Dupi Tila aquifer. Active aquifer is unconformably overlying Minor groundwater source in the vicinity; 2nd aquifer with lower hydraulic conductivity Coal beds are overlain by Dupi Tila aquifer, major GW source Regional aquifer Dupi Tila on top Overburden/Roof materials (preferably Impervious) 150–200 m cover of hard, compacted, impervious Gondwana sandstone 140 m thick Permian Gondwana sandstone (aquifer) in hydraulic continuity with the seam VI 184 m Gy mudstone, sandstone and pebble interbeds of Surma group, lower permeability >300 m of poorly consolidated water- bearing sandy layer forming Dupi Tila aquifer unconformably overlain by loosely consolidated Upper Tertiary Dupi Tila sandy formation Hydraulic head 108 bar Seam dipping 5°–15° 12° (seam VI) 13.4° (seam-II) Reserve (Million Ton) 1053 390 685 865 572 Cited [ 1 , [83] , [84] , [85] ] [ 73 , 86 ] [ 72 , 87 ] [ 75 , 88 ] [ …”
Section: Methodsmentioning
confidence: 99%