Characteristics and distribution of sweet spots in ultra-deep basement reservoirs in compressional tectonic settings: insights from the Northern Qaidam Basin

Ultra-deep basement gas reservoirs typically exhibit complex lithology, strong heterogeneity, and a lack of unified classification criteria, posing significant challenges for high-quality reservoir prediction. This study focuses on the Devonian basement of the T Block in the Kunteyi Gas Field, Qaidam Basin, at depths exceeding 6000 m. An integrated approach combining thin-section petrography, petrophysical measurements, image logging, gas productivity tests, principal component analysis, wave impedance inversion, and co-kriging modeling was employed to systematically characterize the reservoir and predict sweet spot distribution. The basement is dominated by low-potassium granitic gneiss and plagioclase gneiss, with reservoir space comprising a dual-porosity system of tectonic fractures and dissolution pores. Matrix porosity averages ~ 4% (1–6%), and fracture density typically ranges from 3 to 4 fractures/m (0.5–6 fractures/m), with a dominant NE 30° strike nearly orthogonal to the regional NW-trending major faults. A three-tier reservoir classification scheme (Types I-III) based on lithology, porosity, and fracture intensity correlates strongly with gas productivity. Sweet spots were quantitatively predicted using thresholds of porosity ≥ 3%, fracture density ≥ 4 fractures/m, and gas saturation ≥ 50%. The sweet spots exhibit distinct vertical zonation: they form large, NE-trending continuous zones in the 0–100 m interval; migrate to structural flanks as arcuate belts in the 100–200 m interval; disintegrate into isolated patches in the 200–300 m interval; and diminish to scattered remnants below 300 m. Notably, sweet spots are predominantly distributed within 200–500 m of major faults, representing a critical equilibrium window where fracture intensity is sufficient for storage and flow, yet fault damage is not severe enough to compromise gas preservation. This study provides a quantitative evaluation framework and a practical fault-offset criterion for sweet spot prediction in ultra-deep basement gas reservoirs in compressional tectonic settings.

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Journal
Scientific Reports
Published
2026-07-30
DOI
https://doi.org/10.1038/s41598-026-64072-z
Primary Topic
Geological formations and processes
Type
article
Field-Weighted Citation Impact
0.00

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article

Characteristics and distribution of sweet spots in ultra-deep basement reservoirs in compressional tectonic settings: insights from the Northern Qaidam Basin

Ahmed E. Radwan, Ying Wu, Xiaofei Ru, Shuai Yin
Scientific Reports
Geological formations and processes
article

Characteristics and distribution of sweet spots in ultra-deep basement reservoirs in compressional tectonic settings: insights from the Northern Qaidam Basin

Ahmed E. Radwan, Ying Wu, Xiaofei Ru, Shuai Yin
article en

Abstract

Ultra-deep basement gas reservoirs typically exhibit complex lithology, strong heterogeneity, and a lack of unified classification criteria, posing significant challenges for high-quality reservoir prediction. This study focuses on the Devonian basement of the T Block in the Kunteyi Gas Field, Qaidam Basin, at depths exceeding 6000 m. An integrated approach combining thin-section petrography, petrophysical measurements, image logging, gas productivity tests, principal component analysis, wave impedance inversion, and co-kriging modeling was employed to systematically characterize the reservoir and predict sweet spot distribution. The basement is dominated by low-potassium granitic gneiss and plagioclase gneiss, with reservoir space comprising a dual-porosity system of tectonic fractures and dissolution pores. Matrix porosity averages ~ 4% (1–6%), and fracture density typically ranges from 3 to 4 fractures/m (0.5–6 fractures/m), with a dominant NE 30° strike nearly orthogonal to the regional NW-trending major faults. A three-tier reservoir classification scheme (Types I-III) based on lithology, porosity, and fracture intensity correlates strongly with gas productivity. Sweet spots were quantitatively predicted using thresholds of porosity ≥ 3%, fracture density ≥ 4 fractures/m, and gas saturation ≥ 50%. The sweet spots exhibit distinct vertical zonation: they form large, NE-trending continuous zones in the 0–100 m interval; migrate to structural flanks as arcuate belts in the 100–200 m interval; disintegrate into isolated patches in the 200–300 m interval; and diminish to scattered remnants below 300 m. Notably, sweet spots are predominantly distributed within 200–500 m of major faults, representing a critical equilibrium window where fracture intensity is sufficient for storage and flow, yet fault damage is not severe enough to compromise gas preservation. This study provides a quantitative evaluation framework and a practical fault-offset criterion for sweet spot prediction in ultra-deep basement gas reservoirs in compressional tectonic settings.

Scientific Reports
Wrocław University of Science and Technology (PL), Xi'an Shiyou University (CN), University of Petroleum (ID), AGH University of Krakow (PL)
National Natural Science Foundation of China, China National Petroleum Corporation
Life below water
Openalex Percentile: Top 10%
Geological formations and processes
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