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Sedimentary Facies and Geochemical Signatures of the Khewra Sandstone: Reconstructing Cambrian Paleoclimates and Paleoweathering in the Salt Range, Pakistan

  • Abdul Bari Qanit
  • , Shahid Iqbal
  • , Azharul Haq Kamran
  • , Muhammad Idrees
  • , Benjamin Sames
  • , Michael Wagreich

Veröffentlichungen: Beitrag in FachzeitschriftArtikelPeer Reviewed

Abstract

Red sandstones of the Cambrian age are globally distributed and represent an important sedimentation phase during this critical time interval. Their sedimentology and geochemistry can provide key information about the sedimentation style, paleoclimatic conditions, and weathering trends during the Cambrian. In the Salt Range of Pakistan, the Khewra Sandstone constitutes the Lower Cambrian strata and consists of red–maroon sandstones with minor siltstone and shale in the basal part. Cross-bedding, graded bedding, ripple marks, parallel laminations, load casts, ball and pillows, desiccation cracks, and bioturbation are the common sedimentary features of the formation. The sandstones are fine to medium to coarse-grained with subangular to subrounded morphology and display an overall coarsening upward trend. Petrographic analysis indicates that the sandstones are sub-arkose and sub-lithic arenites, and dolomite and calcite are common cementing materials. X-ray Diffraction (XRD) analysis indicates that the main minerals in the formation are quartz, feldspars, kaolinite, illite, mica, hematite, dolomite, and calcite. Geochemical analysis indicates that SiO2 is the major component at a range of 53.3 to 88% (averaging 70.4%), Al2O3 ranges from 3.1 to 19.2% (averaging 9.2%), CaO ranges from 0.4 to 25.3% (averaging 7.4%), K2O ranges from 1.2 to 7.4% (averaging 4.8%), MgO ranges from 0.2 to 7.4% (averaging 3.5%), and Na2O ranges from 0.1 to 0.9% (averaging 0.4%), respectively. The results of the combined proxies indicate that the sedimentation occurred in fluvial–deltaic settings under overall arid to semi-arid paleoclimatic conditions with poor to moderate chemical weathering. The Khewra Sandstone represents the red Cambrian sandstones on the NW Indian Plate margin of Gondwana and can be correlated with contemporaneous red sandstones in the USA, Europe, Africa, Iran, and Turkey (Türkiye).

OriginalspracheEnglisch
Aufsatznummer789
FachzeitschriftMinerals
Jahrgang15
Ausgabenummer8
DOIs
PublikationsstatusVeröffentlicht - Aug. 2025

Fördermittel

Fieldwork Funding by Higher Education Commission (HEC) of Pakistan, Geochemical analysis Funding by Austrian Academy of Sciences through the project “NOMAJU”, under the framework of UNESCO-IGCP projects IGCP-710 and IGCP-732, Open Access Funding by the University of Vienna.

ÖFOS 2012

  • 105105 Geochemie
  • 105121 Sedimentologie
  • 105123 Stratigraphie

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