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X-Ray differaction analysis for the interpretation of clay minerals paragenesis in the neogene sediments of mang and vicinity sub himalayas pakistan

Author

Listed:
  • Muhammad Yasin

    (Institute of Geology, University of Azad Jammu and Kashmir, Muzaffarabad, Pakistan)

  • Muhammad Ibrahim

    (Plant operator at Fauji Fertilizer Company Limited, Pakistan.)

Abstract

The Neogene sediments were interpreted to understand the clay mineral paragenesis in rocks using x-ray differaction technique. The process was conducted with an x-ray diffractometer, Anode = Cu (Cu Kᾳ = 1.541871 A? ), Filter = Ni, Current = 15 mA and Voltage = 35 kv. The clay mineral assemblages in the rocks indicates that the neogene sediments were derived from the preexisting sedimentary, metasedimentary, metamorphics and igneous rocks and formed in different climes in the continental environment. The illite crystallinity (IC) value (0.2165 Δ°2θ CuKα) in the area correspond exactly with the epizonal metamorphic conditions.

Suggested Citation

  • Muhammad Yasin & Muhammad Ibrahim, 2017. "X-Ray differaction analysis for the interpretation of clay minerals paragenesis in the neogene sediments of mang and vicinity sub himalayas pakistan," Earth Sciences Malaysia (ESMY), Zibeline International Publishing, vol. 1(1), pages 32-35, January.
    • Handle: RePEc:zib:zbesmy:v:1:y:2017:i:1:p:32-35
    DOI: 10.26480/esmy.01.2017.32.35
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    Cited by:

    1. Enayatollah Emami Meybodi & Syed Khaliq Hussain, 2022. "The Karstic Geomorphology In The Dolomite Of Drinjal Formation In Central Iran (Case Study Saddat Sirize Iron Mine)," Earth Sciences Malaysia (ESMY), Zibeline International Publishing, vol. 6(1), pages 11-14, January.

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