Volume 45 Issue 5
Oct.  2026
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SHI Huanshan,HU Wangshui,LI Tao,et al. Joint mercury intrusion porosimetry-NMR evaluation and sweet spot identification of high-clay siltstone interlayers: A case study of Well PⅡ in Qing-1 Member, Gulong Depression[J]. Bulletin of Geological Science and Technology,2026,45(5):95-111 doi: 10.19509/j.cnki.dzkq.tb202605039
Citation: SHI Huanshan,HU Wangshui,LI Tao,et al. Joint mercury intrusion porosimetry-NMR evaluation and sweet spot identification of high-clay siltstone interlayers: A case study of Well PⅡ in Qing-1 Member, Gulong Depression[J]. Bulletin of Geological Science and Technology,2026,45(5):95-111 doi: 10.19509/j.cnki.dzkq.tb202605039

Joint mercury intrusion porosimetry-NMR evaluation and sweet spot identification of high-clay siltstone interlayers: A case study of Well PⅡ in Qing-1 Member, Gulong Depression

doi: 10.19509/j.cnki.dzkq.tb202605039
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  • Author Bio:

    E-mail:13288014@qq.com

  • Corresponding author: E-mail:ltm817@163.com
  • Received Date: 19 Nov 2025
  • Accepted Date: 26 May 2026
  • Rev Recd Date: 19 May 2026
  • Available Online: 22 Jun 2026
  • Objective 

    Continental interlayer-type shale oil in China has become a critical strategic resource for increasing reserves and production. High-clay siltstone interlayers in the First Member of Qingshankou Formation (Qing-1 Member) of Gulong Depression, Songliao Basin, are important carriers of shale-oil micro-migration and local accumulation. Nevertheless, controlled jointly by clay minerals, fine throats, and heterogeneity in pore-throat connectivity, high-clay siltstone interlayers within shale-oil sequences commonly show distinct oil-bearing characteristics but poor fluid mobility. Existing studies lack quantitative coupling relationships between pore-throat parameters derived from high-pressure mercury intrusion porosimetry (MIP) and fluid-mobility indicators obtained from nuclear magnetic resonance (NMR) for such high-clay interlayers, and sweet spot classification still largely relies on empirical judgment. This study targets high-clay siltstone interlayers of the Qing-1 Member in the Gulong Depression, Songliao Basin. Under the constraints of the same well and identical lithofacies, this study aims to clarify the intrinsic relationship between pore-throat structure and fluid mobility, establish a quantitative sweet spot identification criterion, and mitigate misjudgment risks caused by merely using oil-bearing indicators for reservoir evaluation.

    Methods 

    Ten groups of paired core samples from Well PⅡ were collected, and the mineral difference index (MDI)≤15% was used to ensure mineralogical comparability between MIP and NMR subsamples. Integrated laboratory tests, including high-pressure mercury intrusion porosimetry, two-dimensional NMR under original oil-bearing conditions, and centrifugal NMR after oil washing and simulated formation-water saturation, were conducted to obtain key parameters such as median pore-throat radius r50, sorting coefficient σ, mercury withdrawal efficiency, transverse relaxation time T2 cutoff value, movable-fluid saturation SMF, and saturated-state geometric mean of T2. A composite movable-oil index (CMOI=So×SMF/100) was constructed to jointly characterize the contributions of both oil-bearing characteristics and fluid mobility. Based on micro-scale computed tomography (CT) scanning and scanning electron microscopy (SEM) observations, microscopic mechanisms of throat narrowing and pore-throat connectivity impairment induced by clay film coating and bridging infill were revealed to explain the statistical patterns observed in the macroscopic experiments.

    Results 

    For high-clay siltstone interlayers, pore-throat parameters from MIP showed significant correlations with NMR mobility indicators. With increasing clay content, r50 decreased, while SMF, CMOI, and the saturated-state geometric mean of T2 decreased simultaneously. Affected by clay-bound water, the T2 cutoff value was not suitable for cross-sample comparison. Instead, the saturated-state geometric mean of T2 was more suitable for characterizing differences in sample mobility. Based on the analysis of well-interval samples, a empirical sweet spot identification combination was proposed: r50>0.4 μm, SMF>40% and CMOI≥20%. Four evaluation zones (Type A-D) were further defined on the SMF-r50 cross-plot. The samples occurred only in types A, B, and D, with no Type-C samples observed. Type-B samples were characterized by large pore-throat sizes but limited mobility, reflecting the reservoir characteristics of "large pore-throat size does not guarantee high mobility".

    Conclusion 

    Constrained by the sample size and sampling scope, the proposed identification criteria are only applicable to the same-lithofacies interval of the Qing-1 Member within Well PⅡ. Further sample expansion and verification are required for threshold calibration. The joint discrimination scheme combining CMOI and SMF-r50 can effectively distinguish oil-bearing reservoirs with limited mobility, and it can be applied to relative ranking and sweet spot classification of analogous siltstone interlayers within this well interval.

     

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