Sedimentary geology and biostratigraphy of the Mianwali Formation, Kala Chitta Range, Northern Pakistan

Authors

  • Kaleem Akhtar Qureshi Geological Survey of Pakistan, 16-G, Model Town, Lahore
  • Ali Nasir Fatmi Geological Survey of Pakistan, 16-G, Model Town, Lahore
  • Riaz Ahmed Sheikh Institute of Geology, Punjab University, Lahore - 54590
  • Aftab Ahmad Butt Institute of Geology, Punjab University, Lahore - 54590

DOI:

https://doi.org/10.3126/jngs.v19i0.32093

Keywords:

Macrofacies analysis, Biostratigraphy, Mianwali Formation, Kala Chitta range, Northern Pakistan

Abstract

Microfacies analysis and ammonite biostratigraphy of the Mianwali Formation of the Kala China Range were worked out on the basis of stratigraphic sections from Chak Jabbi and Bagh. Four microfacies were identified from the Chak Jabbi section while amrnonite biostratigraphy was studied from both the sections. Filamentous bivalves in micrite deposited along a shelf margin below normal wave base represent the first microfacies. The second microfacies contains bioclastic wackestone deposited in an open marine environment of normal salinity. The third microfacies consists of lime mudstone formed in a stressed environment of lagoonal conditions, whereas the fourth microfacies of dolomitised carbonate mudstone was formed by the diagenetic dolomitisation of the third microfacies.

The new collection of ammonites includes Arctoceras tuberculatum, Anakashmirites aff. evolutus, Meekoceras gracilitatis, Stephanites sp., Pseudoceltites sp., Subvishnuites aff. welteri, Arnautoceltites sp., Owemtes sp. indet, Subvishnuites aff. enveris, Pseudosageceras sp. indet, Paranannites sp., Subcolumbites sp., Anasibrites sp., and Pseudaspidites sp, confirming the already known Sctythian age of the Mianwali Formation.

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Published

1999-12-01

How to Cite

Qureshi, K. A., Fatmi, A. N., Sheikh, R. A., & Butt, A. A. (1999). Sedimentary geology and biostratigraphy of the Mianwali Formation, Kala Chitta Range, Northern Pakistan. Journal of Nepal Geological Society, 19, 49–57. https://doi.org/10.3126/jngs.v19i0.32093

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