Integrated sedimentological and geochemical characterization of the Silurian Qalibah Formation in central Saudi Arabia: Implications to paleoenvironmental reconstruction and organic richness evaluation

Mutasim Osman, Korhan Ayranci, Khairul Azlan Mustapha*, Eduardo Gramajo, Rached Maurice Rached, Thomas Finkbeiner, Mahmoud Mowafi

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

Abstract

Unconventional hydrocarbon reservoirs are challenging due to their vertical and lateral heterogeneities. The Silurian Qalibah Formation in Saudi Arabia comprising of the Qusaiba and Sharawra members, serves as a prime example. This study investigates reservoir heterogeneity and variations in depositional conditions to produce a high-resolution chemozonation of the Qalibah Formation. Mineralogical and elemental compositions were determined using X-ray fluorescence (XRF) and X-ray diffraction (XRD), while organic matter characterization was performed using Rock-Eval pyrolysis. Three facies were identified: laminated grey-red mudstones in the Qusaiba Member, heterolithic sandstone-mudstone alternation in the lower Sharawra Member, and thickening upward fine sandstones in the upper Sharawra Member. Clay minerals dominate the Qusaiba Member (50 %), while quartz, mica, and K-feldspars prevail in the Sharawra Member. Organic matter is in early maturation stage with poor-to-fair total organic carbon (TOC) content, averaging 0.2 wt% in the Qusaiba Member and 0.05 wt% in the Sharawra Member. Detrital influx proxies indicate higher sedimentation rates in the Sharawra Member compared to the Qusaiba Member. Paleoclimatic proxies suggest humid to semi-arid conditions in the Qusaiba Member and semi-arid to arid conditions in the Sharawra Member. Paleomarine proxies consistently reveal brackish to saline and suboxic to oxic conditions. Five chemozones were established: three in the Qusaiba Member (Q-1: Ti/P depletion; Q-2: elevated TOC; Q-3: spiking Sr/Ba) and two in the Sharawra Member (S-1: lower Zr/Al and Sr/Cu than S-2). This chemozonation highlights spatial-temporal geochemical variability, offering insights into depositional dynamics and reservoir heterogeneity. The framework supports chemo-steering applications to optimize drilling, enhance reservoir targeting, and improve hydrocarbon recovery in analogous unconventional systems.

Original languageEnglish
Article number107498
JournalMarine and Petroleum Geology
Volume181
DOIs
StatePublished - Nov 2025

Bibliographical note

Publisher Copyright:
© 2025 Elsevier Ltd

Keywords

  • Geochemistry
  • Heterogeneity
  • Qalibah formation
  • Qusaiba member
  • Silurian
  • Unconventional reservoir

ASJC Scopus subject areas

  • Oceanography
  • Geophysics
  • Geology
  • Economic Geology
  • Stratigraphy

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