Marine Geophysical Research

, Volume 37, Issue 3, pp 207–228 | Cite as

Sequence stratigraphic analysis of Eocene Rock Strata, Offshore Indus, southwest Pakistan

  • Natasha KhanEmail author
  • Khaista Rehman
  • Sajjad Ahmad
  • Jamil Khokher
  • M. Iqbal Hajana
  • M. Hanif
Original Research Paper


In this study, seismic data from two wells (Pak G2-1 and Indus Marine-1C) and age diagnostic larger benthic foraminifera (LBF) within drill cuttings has been used for the first time to identify depositional sequences within the carbonates in the Offshore Indus Basin, Pakistan. The Offshore Indus is tectonically categorized as a passive continental margin where carbonates occur as shelf carbonates in the near offshore and on volcanic seamounts in deeper waters. Seismic data analysis has indicated the presence of minor faults and carbonate buildups above the igneous basement in the south. Patterns of the seismic reflections enabled definition of three seismic facies units identified as: Unit 1 basement, represented by chaotic, moderate amplitude reflection configuration; while parallel bedding and the drape of overlying strata is typical character of Unit 2, carbonate mound facies. The younger Miocene channels represent Unit 3. The diagnosis of Alveolina vredenburgi/cucumiformis biozone confirmed the Ilerdian (55–52 Ma) stage constituting a second order cycle of deposition for the Eocene carbonates (identified as Unit 2). The carbonate succession has been mainly attributed to an early highstand system tract (HST). The environmental conditions remained favorable leading to the development of keep-up carbonates similar to pinnacle buildups as a result of aggradation during late transgressive system tract and an early HST. The carbonate sequence in the south (Pak G2-1) is thicker and fossiliferous representing inner to middle shelf depths based on fauna compared to the Indus Marine-1C in the north, which is devoid of fossils. Three biozones (SBZ 5, SBZ 6 and SBZ 8) were identified based on the occurrence of LBF. The base of the SBZ 5 zone marks the larger foraminifera turnover and the Paleocene–Eocene (P–E) boundary. The LBF encountered in this study coincides with earlier findings for the P–E boundary. Our findings indicate that the entire Ilerdian stage ranges from 55.5 to 52 Ma that was the episode of warmer water conditions on the carbonate shelves leading to the diversification of K-strategist larger foraminifera. The larger foraminiferal assemblage encountered in this study confirms the findings. The possible indication of stratigraphic-combination traps, revealed as reflection terminations, make carbonate mounds in the south a potential exploration target.


Offshore Seismic stratigraphy Biostratigraphy Ilerdian stage Carbonates Seamounts Canyons Arabian Sea 



Directorate General of Petroleum Concessions (DGPC) and Hydrocarbon Development Institute of Pakistan (HDIP) are highly acknowledged for providing seismic data and well samples for this research. We are thankful to National Centre of Excellence in Geology and Department of Geology, University of Peshawar, Pakistan for providing research facilities. Thanks are also extended to Rashid Messiah (Rock cutter, Department of Geology, University of Peshawar) for his kind help in preparation of thin sections. We are also thankful to the anonymous reviewers for their suggestions to improve the manuscript.


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Copyright information

© Springer Science+Business Media Dordrecht 2016

Authors and Affiliations

  • Natasha Khan
    • 1
    Email author
  • Khaista Rehman
    • 1
  • Sajjad Ahmad
    • 2
  • Jamil Khokher
    • 3
  • M. Iqbal Hajana
    • 4
  • M. Hanif
    • 1
  1. 1.National Center of Excellence in GeologyUniversity of PeshawarPeshawarPakistan
  2. 2.Department of GeologyUniversity of PeshawarPeshawarPakistan
  3. 3.MOL Pakistan Oil and Gas B.V.IslamabadPakistan
  4. 4.3D Seismic Lab, School of Earth and Ocean SciencesCardiff UniversityCardiffUK

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