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November 14, 2025GeosciencesOpen Access

The Structural and Diagenetic Coupling Controls the Distribution of Deep Carbonate Rock Reservoirs in the Southern of Tahe Oilfield, Tarim Basin

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Authors

YWYan WangHCHua-xin ChenYLYongli Liu

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Overview

Analysis reveals factors affecting formation water and fluid migration in Tarim Basin, suggesting implications for hydrocarbon exploration.

Key Points

  • Reservoir development is driven by the interplay of geological faulting and distinct diagenetic fluids, with evidence from geochemical data.
  • Four fluid types identified include meteoric water, formation water, hydrothermal fluids, and mixed fluids, impacting migration pathways.
  • Analysis using cores and 3D seismic interpretation illustrates historical faulting influences on reservoir characteristics.
  • Understanding these controls may enhance predictions for deep carbonate rock reservoirs and inform hydrocarbon exploration strategies.

Cite This Study

Wang et al. (2025) studied this question.

synapsesocial.com/papers/692519acc0ce034ddc35434ahttps://doi.org/10.3390/geosciences15110435
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Also Consider

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  1. 1Effect of Multi-Stage Strike Slip Faults and Fluids Effect on the Origin and Evolution of a Deep Carbonate Reservoir in the Southern of Tahe Oilfield, Tarim Basin2025
  2. 2The spatial and geological characteristics of fault- and paleokarst-controlled carbonate-hosted reservoirs in the Tabei Uplift, Tarim Basin, China2024 · 7 citations
  3. 3Fluid Types and Geologic Models for Karst Reservoir Development Within the Penglaiba–Lower Yingshan Formations, Ordovician, Northern Tarim Basin2026
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  5. 5Strike–Slip Fault-Associated Paleokarst Systems: A Comparison Between the Tarim Basin, NW China, and Monts de Vaucluse, SE France2026