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Sediments analysis of eastern makran coast line area of Pakistan by X-Ray diffraction

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Research Paper 01/07/2016
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Sediments analysis of eastern makran coast line area of Pakistan by X-Ray diffraction

Syed Waseem Haider
J. Bio. Env. Sci.9( 1), 11-19, July 2016.
Certificate: JBES 2016 [Generate Certificate]
Key: Makran Coastal areaMineralX-Ray Diffraction

Abstract

Sediment are mechanically and/or chemically weathered rocks, they are unconsolidated materials. Present Research investigation conducted on the sediment of Coast line area of Markran. Six major areas selected for the collection of sediment sample which are Sur Bandar, Koh Mehdi, Ganz, Pishukan, Gwader and Jiwani. Total sediment sample stations are eighteen, out of which one  station on the Sur Bandar, one station on Koh Mehdi, Three stations on Ganz, Three stations on Pishukan, Three stations on Gwader East Bay, Five stations on Gwader West Bay and Two stations on Jiwani.  Latest scientific instrument and technique X-Ray Diffraction (XRD) used in this time for investigation of Minerals. Quartz, Kaolinites, Calcite are the common mineral found during this study. Calcite and Quartz are found throughout the targeted area of the coastal belt and a major area has Kaolinites during this research. Baratovite found in some places. These types of mineral into sediment are normally due to the weathering of pre-existing rock and transport by running water in rivers, Ocean currents. Other less common factors uses for transportation of sediments are wind, glaciers and landslides. River sediments originate by the erosion process of near surface, exposed igneous, metamorphic or sedimentary rock. The sediments are then deposited and form sedimentary rock.

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Akhtar MK, Shuhab DK, Huseyin B, Aimal KK. 2013. Newly discovered mud volcanoes in the Coastal Belt of Makran, Pakistan-tectonic implications: Arab Journal of Geosciences 11, 4899-4909. DOI 10.1007/S12517-013-1135-7.

Baloch AH, Rehman H, Saeed M, Kalhoro MA, Buzdar MA.  2014. The Curious Case of Mangroves Forest at the Sonmiani bay Area, Lasbela District, Pakistan: A review. Lasbela University Journal of Science and Technology 3, 61-74.

Borreswar RC. 1957. Beach erosion and concentration of heavy minerals, Journal sedimentary Petrology 27, 143-147.

Deslisle G, Rad VU, Andruleit H, Daniels CHV, Tabrez AR, Inam A. 2002. Active mud volcanoes on and offshore eastern Makran, Pakistan. International Journal of Earth Sciences (Geologische Rundschas) 81, 93-110.  DOI  10.1007/ S005310 100203.

Fe. BE (Ed).  1976. Chemistry of soil: Second edition, Third Indian Reprint, Oxford and IBH Publishing Co., New Delhi.

Grim RE. 1968. Clay Mineralogy: 2nd Edition, McGraw Hill., New Delhi 45-156.

Hunting Survey Corporation Ltd. 1961. Reconn aissance geology of part of West Pakistan. Miracle Press. Ottawa, Ontario, Canada 1-550.

Kassi AM, Khan AS, Kasi AK. 2007. Newly proposed Cretaceous-Palaeocene lithostratigraphy of the Ispikan-Wakai area, Southwestern Makran, Pakistan. Pakistan Journal of  Himalayan  Earth Sciences  40, 25-31.

Kassi AM, Khan AS, Kelling G, Kasi AK. 2011. Facies and cyclicity within the Oligocene-Early Miocene Panjgur formation, Khojak – Panjgur Submarine Fan Complex, south-west Makran, Pakistan. Journal  Asian Earth Sciences 41(6), 537-550.

Kim H, Tin. 1978. Principle of Soil Science: 2nd Edition 145-258.

Kumar PD, Wang Chi. 1984. Processes of selective grain transport and the formation of placers on beach.  Journal Geology  92, 637-655.

Leggett JK, Platt J. 1984. Structural features of the Makran fore-arc on Landsat imagery. In: Haq BU, Milliman JD (eds) Marine Geology and Oceanography of Arabian Sea and Coastal Pakistan. Van Nostrand Reinhold, New York 33-43.

Platt JP, Leggett JK, Alam S. 1988. Slip vectors and fault mechanics in the Makran accretionary wedge, southwest Pakistan. Journal of Geophysical Research 93(B7), 7955-7973.

Platt JP, Leggett JK, Young J, Raza H, Alam S. 1985. Large-scale underplating in the Makran accretionary prism, southwest  Pakistan. Geology  13, 507-511.

Rad UV, Berner U, Delisle G, Dosse-Rolinski H, Fechner N, Linke P, Luckge A, Roeser HA, Schmaljohann R, Wiedicke. 2000. Gas and Fluid venting at the Makran accretionary wedge off Pakistan. (Geo-Marine letter 2000) Springer-Verlag 2000 20, 10-19.

Rao RG, Sahoo P, Panda NK. 2001. Heavy mineral sand deposit of Orissa. Exploration and Research for atomic Minerals 13, 23-52.

Smith HG. 1952. Minerals and Microscope, Thomas Murby and Co. London.

White RS. 1983 The Makran accretionary prism, in: Bally, A.W., (Ed.), Seismic Expression of Structural Styles. American Association of Petroleum Geologists, Studies Geology 15, 3.4.2-178 – 3.4.2-182.

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