International Journal of Economy, Energy and Environment

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

Received: 09 July 2016    Accepted: 22 July 2016    Published: 28 October 2016
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Abstract

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 (CaCO3). The average chemical property of limestone is 44% CaO, 10% SiO2, 1% Fe2O3 and 2% Al2O3. 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.

DOI 10.11648/j.ijeee.20160102.13
Published in International Journal of Economy, Energy and Environment (Volume 1, Issue 2, October 2016)
Page(s) 34-39
Creative Commons

This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Calcareous, Carbonate, Deposits, Fossiliferous, Limestone, Rock

References
[1] Alam, M., K., et al, (1990): Geological map of Bangladesh, Published by, GSB. Bangladesh. Bangladesh Journal of Geology, Vol. 14, P. 1-14.
[2] BMEDC Report, 1976, Economic Feasibility Reports on Limestone Mine, commission of Bangladesh. Exhibition on Petroleum and Mineral Resources of Bangladesh, P. 35-40.
[3] F. J. Pettijohn, (1984): Sedimentary Rocks, Third edition, CBS Publishers and Distributors, Delhi, India
[4] Fried. Krupp Rohstoffe, Find report, First phase, Joypurhat limestone project.
[5] Imam. Badrul, (2005): Energy Resources of Bangladesh. University Grant Commission.
[6] Islam, M, N, (1985): White clay deposits of Bijoypur area, Netrokona district, Bangladesh, Government of the People’s Republic of Bangladesh.
[7] Islam. M. N, (1985): White clay deposits of Bijoypur area, Netrokona district, Bangladesh, Government of the People’s Republic of Bangladesh. Jaypurhat and Limestone Mining & Cement Plant, Jaypurhat, Bogra.
[8] Khan F. H, (1991): Geology of Bangladesh. The university press limited.
[9] Khan, M. R and Muminullah, M., (1980): Stratigraphy of Bangladesh, Seminar and project, Dinajpur, Bangladesh.
[10] Reimann, K. U., (1993): Geology of Bangladesh, Gebruder Borntrager, Berlin.
[11] Reineck. Singh, 1980, Depositional Sedimentary Environment, Springer-Verlag Berlin Heidelberg New York.
[12] Statistical Yearbook of Bangladesh.(2011): Bureau of Statistics, Government of the people’s Republic of Bangladesh.
[13] Uddin, M. N., (1995): Foraminiferal Assemblages and Paleoecology of the Kopili.
[14] Wardell Armstron (1991): Techno-economic feasibility study, Barapukuria coal. Dinajpur.
[15] Zaher, M, A et, al. 1986, Subsurface Geology of the Limestone Deposits of Joypurhat Area, Joypurhat District, Bangladesh, Records of the Geological Survey of Bangladesh., Vol. 4, Part. 4.
[16] Zaher. M. A, Alam. M. K, S. I Chowdhury, (1986): Subsurface geology of the limestone deposits of Joypurhat area, Joypurhat district, Bangladesh, Government of the People’s Republic of Bangladesh.
Author Information
  • Department of Geological Survey of Bangladesh, Pioneer Road Segunbagicha, Dhaka, Bangladesh

  • Department of Geological Survey of Bangladesh, Pioneer Road Segunbagicha, Dhaka, Bangladesh

  • Department of Geological Survey of Bangladesh, Pioneer Road Segunbagicha, Dhaka, Bangladesh

  • Department of Geological Survey of Bangladesh, Pioneer Road Segunbagicha, Dhaka, Bangladesh

  • Department of Geological Survey of Bangladesh, Pioneer Road Segunbagicha, Dhaka, Bangladesh

  • Department of Geological Survey of Bangladesh, Pioneer Road Segunbagicha, Dhaka, Bangladesh

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  • APA Style

    Mohammed Masum, Nehal Uddin, Nazwanul Haque, Nuruzzaman Sabuj, Mohammad Shahariar Hasan, et al. (2016). Limestone Deposits and Its Economic Importance at Panchbibi Area of Joypurhat District, Bangladesh. International Journal of Economy, Energy and Environment, 1(2), 34-39. https://doi.org/10.11648/j.ijeee.20160102.13

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    ACS Style

    Mohammed Masum; Nehal Uddin; Nazwanul Haque; Nuruzzaman Sabuj; Mohammad Shahariar Hasan, et al. Limestone Deposits and Its Economic Importance at Panchbibi Area of Joypurhat District, Bangladesh. Int. J. Econ. Energy Environ. 2016, 1(2), 34-39. doi: 10.11648/j.ijeee.20160102.13

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    AMA Style

    Mohammed Masum, Nehal Uddin, Nazwanul Haque, Nuruzzaman Sabuj, Mohammad Shahariar Hasan, et al. Limestone Deposits and Its Economic Importance at Panchbibi Area of Joypurhat District, Bangladesh. Int J Econ Energy Environ. 2016;1(2):34-39. doi: 10.11648/j.ijeee.20160102.13

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  • @article{10.11648/j.ijeee.20160102.13,
      author = {Mohammed Masum and Nehal Uddin and Nazwanul Haque and Nuruzzaman Sabuj and Mohammad Shahariar Hasan and Rubel Sheik},
      title = {Limestone Deposits and Its Economic Importance at Panchbibi Area of Joypurhat District, Bangladesh},
      journal = {International Journal of Economy, Energy and Environment},
      volume = {1},
      number = {2},
      pages = {34-39},
      doi = {10.11648/j.ijeee.20160102.13},
      url = {https://doi.org/10.11648/j.ijeee.20160102.13},
      eprint = {https://download.sciencepg.com/pdf/10.11648.j.ijeee.20160102.13},
      abstract = {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 (CaCO3). The average chemical property of limestone is 44% CaO, 10% SiO2, 1% Fe2O3 and 2% Al2O3. 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.},
     year = {2016}
    }
    

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  • TY  - JOUR
    T1  - Limestone Deposits and Its Economic Importance at Panchbibi Area of Joypurhat District, Bangladesh
    AU  - Mohammed Masum
    AU  - Nehal Uddin
    AU  - Nazwanul Haque
    AU  - Nuruzzaman Sabuj
    AU  - Mohammad Shahariar Hasan
    AU  - Rubel Sheik
    Y1  - 2016/10/28
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    DO  - 10.11648/j.ijeee.20160102.13
    T2  - International Journal of Economy, Energy and Environment
    JF  - International Journal of Economy, Energy and Environment
    JO  - International Journal of Economy, Energy and Environment
    SP  - 34
    EP  - 39
    PB  - Science Publishing Group
    SN  - 2575-5021
    UR  - https://doi.org/10.11648/j.ijeee.20160102.13
    AB  - 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 (CaCO3). The average chemical property of limestone is 44% CaO, 10% SiO2, 1% Fe2O3 and 2% Al2O3. 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.
    VL  - 1
    IS  - 2
    ER  - 

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