1996
DOI: 10.1016/0264-3707(96)00022-1
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The crustal dynamics and the tectonic trends in the Bengal Basin

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Cited by 41 publications
(24 citation statements)
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“…of aerial extension which is at least 100m in thickness reaching 185m in the southern part of the mine area and extends from beneath a shallow covering of Barind clay residuum to its geologically unconformable contact with the groundwater measures [1]. The Dupitila formation and Gondwana sandstone, that is known to be hydraulic continuity with the coal seam VI, North Slope of the Platform, Platform Flank Zone represents a major potential hazard to the mine from water inflow [1,25,26]. BCM is an independent Gondwana coal-bearing basin, which is controlled by half-fault Graben and unconformably laid on the denuded Archean Basement Complex [1,26].…”
Section: Hydrogeology Of Barapukuria Coal Basinmentioning
confidence: 99%
See 1 more Smart Citation
“…of aerial extension which is at least 100m in thickness reaching 185m in the southern part of the mine area and extends from beneath a shallow covering of Barind clay residuum to its geologically unconformable contact with the groundwater measures [1]. The Dupitila formation and Gondwana sandstone, that is known to be hydraulic continuity with the coal seam VI, North Slope of the Platform, Platform Flank Zone represents a major potential hazard to the mine from water inflow [1,25,26]. BCM is an independent Gondwana coal-bearing basin, which is controlled by half-fault Graben and unconformably laid on the denuded Archean Basement Complex [1,26].…”
Section: Hydrogeology Of Barapukuria Coal Basinmentioning
confidence: 99%
“…BCM is an independent Gondwana coal-bearing basin, which is controlled by half-fault Graben and unconformably laid on the denuded Archean Basement Complex [1,26]. Based on brilling data, the strata can be divided into four units such as Basement complex, Gondwana group, Dupi Tila Formation and Barind Residuum Clay and their Lithology [25,26], average thickness and hydrology have been shown in Table 1. …”
Section: Hydrogeology Of Barapukuria Coal Basinmentioning
confidence: 99%
“…Flooding of the mine from breaches in the Upper Dupi Tila aquifer occurred frequently during the development of the mine in 1998. When the mining walls had been extended to a total distance Khan, 1991;Khan and Chouhan, 1996). of about 1200 m, roof pressure increased dramatically and a small amount of water flowed into the mine from several locations along the roof.…”
Section: Introductionmentioning
confidence: 99%
“…These three plates form three major tectonic zones in Bangladesh ( Fig. 1): (i) a platform flank zone in the west named the Dinajpur Shield and Platform, (ii) a central deeper basin, the Bengal Basin, and (iii), the folded belt in the east, known as the ChittagongTripura Fold Belt (Khan, 1991;Khan and Chouhan, 1996;Alam et al, 2003). Each of these zones is distinguished by a unique tectonic and stratigraphic history (Alam et al, 2003).…”
Section: Regional Geologymentioning
confidence: 98%
“…Coal production commenced in 2005 and is continuing at the present time. Khan, 1991;Khan and Chouhan, 1996).…”
Section: Introductionmentioning
confidence: 97%