Source provenance

Yaseen, W., Khan, A.S., Sohail, K., Farooq, U., Usman, M. & Ghani, M. (2019). Modal composition and provenance of Shaigalu Sandstones, Pishin-Katawaz Basin, northern Balochistan, Pakistan. Bahria University Research Journal of Earth Sciences (BURJES), 4(2), 70-77.

Cited by 5 units (5 published) · 2 field-level citations · 1 revision note.

Shaigalu Member of the Khojak Formation (Oligocene) — lithic arenites, recycled-orogen provenance; Pishin-Katawaz succession: Muslim Bagh-Zhob ophiolite (base) → Eocene Nisai Fm (unconformable) → Oligocene-early Miocene Khojak Fm (Murgha Faqirzai + Shaigalu members) → Dasht Murgha Group → Malthanai Fm → Bostan Fm.

This page is the reverse of each unit's per-field citations — it shows exactly what this reference supports, making the dataset's “no source, no fact” rule browsable both ways.

Units citing this source

• Cenozoic Khojak Formation Paleogene

  Listed as a corroborating source for this unit.

• Cenozoic Murgha Faqirzai Formation Paleogene

  Listed as a corroborating source for this unit.

• Mesozoic Muslim Bagh Ophiolite Cretaceous

  Listed as a corroborating source for this unit.

• Cenozoic Nisai Limestone Paleogene
  • Age: Yaseen et al. (2019) and Waliullah et al. (GSP): in the Pishin–Katawaz succession the Nisai Formation is Eocene — a shallow-marine fossiliferous limestone (with shale) that unconformably overlies the Muslim Bagh–Zhob ophiolite at the base of the basin fill, and is in turn overlain by the Oligocene–Early Miocene Khojak Formation. Clarifies the local Eocene age and the basal-ophiolite relationship (an alternative to the curated 'overlies Humai Formation').
• Cenozoic Shaigalu Member Paleogene–Neogene
  AgeLithology