Source provenance

Kasi, A.K., Kassi, A.M., Umar, M., Friis, H., Mohibullah, M. & Manan, R.A. (2018). A Paleogeographic and Depositional Model for the Neogene Fluvial Succession, Pishin Belt, Northwest Pakistan: Effect of Post Collisional Tectonics on Sedimentation in a Peripheral Foreland Setting. Acta Geologica Sinica (English Edition), 92(2), 499-518.

Cited by 3 units (3 published) · 0 field-level citations · 3 revision notes.

Depositional model for the Pishin Belt Neogene fluvial succession.

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Units citing this source

• Cenozoic Bahlol Nika Formation Neogene
  • Geological significance: A unit of the Neogene Dasht Murgha Group fluvial succession of the Pishin Belt (Katawaz peripheral foreland), recording post-collisional molasse sedimentation (Kasi et al. 2018).
• Cenozoic Khuzhobai Formation Neogene
  • Thickness (m): The Khuzhobai Formation is the lowermost unit of the Neogene Dasht Murgha Group: a ~650 m cyclic succession of sandstone with subordinate mudstone (Khuzhobai section), deposited in the Pishin peripheral-foreland fluvial system (Kasi et al. 2018).
• Cenozoic Sra Khula Formation Neogene
  • Lithology: The Sra Khula Formation is a cyclic alternation of sandstone and mudstone conformably above the Khuzhobai Formation, part of the Neogene Dasht Murgha Group fluvial succession of the Pishin Belt (Kasi et al. 2018).