Source provenance

Kasi, A.K., Kassi, A.M., Friis, H., Kakar, M.I. & Manan, R.A. (2014). Clay minerals assemblage in the Neogene fluvial succession of the Pishin Belt, Pakistan: implications for provenance. Journal of Himalayan Earth Sciences, 47(2), 63-73.

Cited by 2 units (2 published) · 4 field-level citations · 2 revision notes.

Defining/using paper for the Neogene Pishin Belt succession: Middle-Upper Miocene Dasht Murgha Group (sub-formations Khuzhobai, Bahlol Nika, Sra Khula; reference section Dasht Murgha Syncline N of Qila Saifullah), Miocene-Pliocene Malthanai Formation (= Multana Fm of Jones 1961; type near Malthanai village), Pleistocene Bostan Formation (Jones 1961). Lithic arenites of recycled/pre-Miocene provenance.

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Units citing this source

• Cenozoic Dasht Murgha Group Neogene
  AgeLithology
  • Member units: Kasi (2012), Kasi et al. (2012, 2014): the group comprises three constituent formations — the Khuzhobai, Bahlol Nika and Sra Khula formations (not yet separate records here); reference section in the Dasht Murgha Syncline north of Qila Saifullah.
• Cenozoic Malthanai Formation Neogene
  AgeLithology
  • Synonyms: = the ‘Multana Formation’ of Jones (1961); renamed the Malthanai Formation by Kasi et al. (2012) after Malthanai village. The Simzai-area report (Ali et al. 2021) spells it ‘Multana’ and gives an Oligocene–Miocene range.