Sedimentology and reservoir characterisation of Lower Jurassic clastic sedimentary rocks, Salt and Trans Indus Ranges, Pakistan: Evidence from petrography, scanning electron microscopy and petrophysics

Abstract In this study, sandstones of the Lower Jurassic Datta Formation in the Salt and Trans‐Indus ranges are investigated regarding composition, diagenesis, provenance and reservoir properties using petrography, scanning electron microscopy and petrophysical analysis. The detrital mineral composition of the Datta Formation indicated that the sandstones are quartzose, lithic‐quartzose, lithic‐feldspatho‐quartzose, lithic‐quartzo‐feldspathic, quartzo‐lithic and feldspatho‐quartzose, primarily from the recycled orogen setting, including the Malani Igneous Suite, the Aravali Range and Nagar Parkar. The Datta Formation has sub‐angular to well‐rounded, fine to coarse and moderate to well‐sorted grains. Numerous diagnostic processes that occurred in the early to late stages of diagenesis, such as compaction, pressure solution, cementation, alteration, dolomitisation and dissolution, are supported by evidence in the Datta Formation. Dissolution, physical compaction, dolomitisation and alteration enhanced the reservoir quality, while pressure solution and cementation reduced the reservoir quality of the Datta Formation. The porosity types detected in the Datta Formation under scanning electron microscopy are vuggy, intracrystalline/intraparticle, dissolution and intercrystalline, with an average petrographic visual porosity of 11%. The petrophysical aspects of the Datta Formation in the Chonai‐01 well and the correlation between four wells indicated that the hydrocarbons had shifted up‐dip towards the Isa‐Khail‐01 well, so it is recommended for drilling because of the greater depositional thickness. The comparison of the Datta Formation with age‐equivalent units in other regions of eastern Tethys provided a better understanding of reservoir heterogeneities that can be applicable in areas with similar geological conditions for future petroleum exploration.

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Publication Details

Journal
The Depositional Record
Published
2024-12-25
DOI
https://doi.org/10.1002/dep2.325
Citations
12
Primary Topic
Hydrocarbon exploration and reservoir analysis
Type
article
Field-Weighted Citation Impact
3.23
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article

Sedimentology and reservoir characterisation of Lower Jurassic clastic sedimentary rocks, Salt and Trans Indus Ranges, Pakistan: Evidence from petrography, scanning electron microscopy and petrophysics

Ihtisham Islam, Nasar Khan, Assimina Antonarakou, Salman Ahmed Khattak et al.
12 citations
The Depositional Record
Hydrocarbon exploration and reservoir analysis
3.23
article

Sedimentology and reservoir characterisation of Lower Jurassic clastic sedimentary rocks, Salt and Trans Indus Ranges, Pakistan: Evidence from petrography, scanning electron microscopy and petrophysics

Ihtisham Islam, Nasar Khan, Assimina Antonarakou, Salman Ahmed Khattak, Hammad Tariq Janjuhah, George Kontakiotis, Waseem Khan, S. Sahaya Jude Dhas
article en
12 citations

Abstract

Abstract In this study, sandstones of the Lower Jurassic Datta Formation in the Salt and Trans‐Indus ranges are investigated regarding composition, diagenesis, provenance and reservoir properties using petrography, scanning electron microscopy and petrophysical analysis. The detrital mineral composition of the Datta Formation indicated that the sandstones are quartzose, lithic‐quartzose, lithic‐feldspatho‐quartzose, lithic‐quartzo‐feldspathic, quartzo‐lithic and feldspatho‐quartzose, primarily from the recycled orogen setting, including the Malani Igneous Suite, the Aravali Range and Nagar Parkar. The Datta Formation has sub‐angular to well‐rounded, fine to coarse and moderate to well‐sorted grains. Numerous diagnostic processes that occurred in the early to late stages of diagenesis, such as compaction, pressure solution, cementation, alteration, dolomitisation and dissolution, are supported by evidence in the Datta Formation. Dissolution, physical compaction, dolomitisation and alteration enhanced the reservoir quality, while pressure solution and cementation reduced the reservoir quality of the Datta Formation. The porosity types detected in the Datta Formation under scanning electron microscopy are vuggy, intracrystalline/intraparticle, dissolution and intercrystalline, with an average petrographic visual porosity of 11%. The petrophysical aspects of the Datta Formation in the Chonai‐01 well and the correlation between four wells indicated that the hydrocarbons had shifted up‐dip towards the Isa‐Khail‐01 well, so it is recommended for drilling because of the greater depositional thickness. The comparison of the Datta Formation with age‐equivalent units in other regions of eastern Tethys provided a better understanding of reservoir heterogeneities that can be applicable in areas with similar geological conditions for future petroleum exploration.

The Depositional RecordVol. 11(2)
INTI International University (MY), Shaheed Benazir Bhutto University (PK), Chinese Academy of Sciences (CN), National and Kapodistrian University of Athens (GR), University of Haripur (PK), Institute of Geochemistry (CN), Institute of Tibetan Plateau Research (CN), University of Chinese Academy of Sciences (CN), University of Malakand (PK), Saveetha University (IN)
Openalex Percentile: Top 7%
Hydrocarbon exploration and reservoir analysis
3.23
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