Source provenance

Iqbal, O., Baig, M.S., Pervez, S. & Siddiqi, M.I. (2018). Structure and Stratigraphy of Rumbli and Panjar Areas of Kashmir and Pakistan with the Aid of GIS. Journal of the Geological Society of India, 91, 57-66.

Cited by 5 units (5 published) · 0 field-level citations · 5 revision notes.

Reviewer-supplied. GIS-aided structural and stratigraphic mapping of the Rumbli-Panjar area in the southern Hazara-Kashmir syntaxis. Documents the Siwalik molasse (Kamlial, Chinji, Nagri, Dhok Pathan, Soan) with local lithofacies, distinguishing petrology (tourmaline in Kamlial; Punjal volcanic clasts in Nagri) and Kashmir-Basin section thicknesses (after Islam 2006).

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Units citing this source

• Cenozoic Chinji Formation Neogene
  • Lithology: Iqbal et al. (2018): in the Rumbli–Panjar area the Chinji Formation is clays, ash-grey sandstone and siltstone with a clay:sandstone ratio of about 70:30 and an absence of Punjal volcanic clasts; contacts with the Kamlial and Nagri formations are gradational.
• Cenozoic Dhok Pathan Formation Neogene
  • Lithology: Iqbal et al. (2018): in the Rumbli–Panjar area the Dhok Pathan Formation is dominantly greenish-grey, massive, medium- to coarse-grained sandstone with siltstone and mudstone. Local section thickness ~1720 m (Kashmir Basin, after Islam 2006).
• Cenozoic Kamlial Formation Neogene
  • Lithology: Iqbal et al. (2018), Rumbli–Panjar area (southern Hazara–Kashmir syntaxis): the Kamlial Formation is sandstone, siltstone and subordinate clays with intraformational conglomerates, exposed at Panjar, Kaloian and Barathian. It is distinguished from the overlying Chinji Formation by dominant tourmaline and from the Nagri Formation by the absence of volcanic clasts; wood fossils, petrified wood and leaf impressions are recorded. Local section thickness ~933 m (Kashmir Basin, after Islam 2006).
• Cenozoic Nagri Formation Neogene
  • Lithology: Iqbal et al. (2018): in the Rumbli–Panjar area (Hazara–Kashmir syntaxis) the Nagri Formation is red to purple, greenish-grey and ash-grey sandstone and siltstone with purple to reddish-brown mudstone. Local section thickness ~1160 m (Kashmir Basin, after Islam 2006).
• Quaternary Soan Formation Quaternary
  • Lithology: Iqbal et al. (2018): in the Rumbli–Panjar area the Soan Formation is dominantly grey, fine- to medium-grained, medium- to thick-bedded sandstone with siltstone and clays; assigned a Pliocene age with a local section thickness ~600 m (Kashmir Basin, after Islam 2006).