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Limestone Deposits and Its Economic Importance at Panchbibi Area of Joypurhat District, Bangladesh

机译:孟加拉国Joypurhat区Panchbibi地区的石灰石矿床及其经济意义

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The study area is located at Panchbibi upazila of Joypurhat District which is in the south-western part of Bangladesh. Tectonically the area lies in the southern slope of Rangpur saddle within the stable Precambrian platform. The investigation work carried out by an exploratory drilling operation with the help of wire line drilling rig. Core samples were collected and subsequently analyzed during the drilling activity. Three limestone layers have been encountered at different depth of this drilling hole which is in between 450 meter to 530 meter below the surface. This limestone is light grey in colour, fossiliferous, sandy in nature, moderately hard and compacted. The outer surfaces of core samples are not smooth. It Composed of mainly (&40%) calcium carbonate (CaCOsub3/sub). The average chemical property of limestone is 44% CaO, 10% SiOsub2/sub, 1% Fesub2/subOsub3/sub and 2% Alsub2/subOsub3/sub. The thickness of limestone is varies from layer to layer where first layer is about 8 m thick and the total thickness of the limestone is about 13 m. The physical and chemical properties of limestone indicated that the quality of limestone is medium to good. Composed of calcareous sands, both skeletal and oolitic, with lesser volume of fine carbonate mud and reef rocks which indicated that the condition of deposition of this limestone is shallow water deposits. It is the most important and widely distributed carbonate rocks which used in many industrial purposes. The limestone deposit of the studied area may utilize at different purposes after extraction like as mainly in manufactures of cement clinkers in the cement factory. Besides it is also used as different construction materials. It should be suggested that more exploratory drilling hole detail geophysical investigation might be done to evaluate the real picture of this deposits.
机译:研究区域位于孟加拉国西南部的Joypurhat区的Panchbibi upazila。从构造上讲,该区域位于稳定的前寒武纪平台内的朗布尔鞍的南坡。在钢丝绳钻机的帮助下,由探索性钻井作业进行的调查工作。收集岩心样品,随后在钻探活动中进行分析。在该钻孔的不同深度处遇到了三个石灰岩层,该深度在地表以下450米至530米之间。这种石灰石是浅灰色的,化石质的,本质上是沙质的,中等硬度和致密性。岩心样品的外表面不光滑。它主要由(> 40%)碳酸钙(CaCO 3 )组成。石灰石的平均化学性质为44%CaO,10%SiO 2 ,1%Fe 2 O 3 和2%Al 2 O 3 。石灰石的厚度随层的不同而变化,其中第一层的厚度约为8 m,而石灰石的总厚度约为13 m。石灰石的物理和化学性质表明,石灰石的质量为中等到良好。由钙质的砂质组成,包括骨架质的和橄榄质的,细碳酸盐泥和礁石的体积较小,这表明该石灰石的沉积条件是浅水沉积。它是最重要且分布广泛的碳酸盐岩,可用于许多工业用途。被研究区域的石灰岩矿床在提取后可能有多种用途,例如主要用于水泥厂的水泥熟料生产中。此外,它还用作不同的建筑材料。应该建议进行更多的探索性的钻孔细节地球物理调查,以评估该矿床的真实情况。

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