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Volume 47 Issue 4
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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2025  >  47(4): 805-819
XU Qinqi, PENG Jun, HE Chengqi, XIA Jingang, LIU Rui, HUANG Wei. Characteristics and genesis analysis of dolomite in Lower Ordovician Penglaiba Formation in Tahe area[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2025, 47(4): 805-819. doi: 10.11781/sysydz2025040805
Citation: XU Qinqi, PENG Jun, HE Chengqi, XIA Jingang, LIU Rui, HUANG Wei. Characteristics and genesis analysis of dolomite in Lower Ordovician Penglaiba Formation in Tahe area[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2025, 47(4): 805-819. doi: 10.11781/sysydz2025040805
shu

Characteristics and genesis analysis of dolomite in Lower Ordovician Penglaiba Formation in Tahe area

doi: 10.11781/sysydz2025040805
  • 1.

    Exploration and Production Research Institute, Northwest Oilfield Company, SINOPEC, Urumqi, Xinjiang 830011, China

  • 2.

    School of Geoscience and Technology, Southwest Petroleum University, Chengdu, Sichuan 610500, China

  • 3.

    Sichuan Provincial Key Laboratory of Natural Gas Geology, Chengdu, Sichuan 610500, China

  • Received Date: 2024-04-20
  • Rev Recd Date: 2025-05-15
  • Publish Date: 2025-07-28
    Abstract
  • The dolomite of the Lower Ordovician Penglaiba Formation is an important successor field for oil and gas exploration in the Tahe oilfield. Clarifying the sedimentary characteristics and genetic mechanisms of the dolomite is of great significance for oil and gas exploration and development in the Tahe oilfield. Based on this, the geological and geochemical characteristics and genetic mechanisms of the dolomite in the Lower Ordovician Penglaiba Formation of the Tahe Oilfield were systematically studied through core description, thin section identification, scanning electron microscopy, cathodoluminescence, and geochemical analyses. The results showed that: (1) The study area was dominated by crystalline dolomite, followed by residual granular dolomite. Mud-microcrystalline dolomite was mainly anhedral. Silty-medium crystalline dolomite was mostly subhedral to euhedral. Medium-coarse crystalline dolomite was predominantly xenomorphic. Residual granular dolomite was mainly composed of silty-fine crystalline dolomite, showing residual intraclastic texture. (2) Cathodoluminescence showed that the mud- microcrystalline dolomite emitted dull blue-purple or dark brown luminescence. Silty dolomite emitted dull purple-red luminescence. Fine-medium crystalline dolomite had a purple core with a bright orange-red rim-shaped band. Medium-coarse crystalline dolomite exhibited purple-red and a bright brown-red rim-shaped luminescent band. (3) Mud-microcrystalline dolomite was mainly enriched in heavy rare earth elements (REE), with large δ18O fluctuations and 87Sr/86Sr ratios close to those in the Early Ordovician seawater, indicating quasi-syngenetic dolomitization by high-salinity evaporative seawater. Residual granular dolomite was mainly characterized by residual intraclastic texture and its genetic mechanism was burial dolomitization. The REE distribution patterns of silty crystalline dolomite and fine-medium crystalline dolomite were similar to those of contemporaneous micrites, which were enriched in heavy REEs with large δ18O fluctuations. The 87Sr/86Sr values were partially higher compared with the strontium isotope values in contemporaneous seawater, indicating products of shallow-medium burial dolomitization superimposed with hydrothermal fluids. Medium-coarse crystalline dolomite was relatively enriched in light rare earth, with negative δ18O values and 87Sr/86Sr values higher than those in contemporaneous seawater, indicating formation by hydrothermal metasomatism related to clastic rock layers.

     

    • All authors declare no relevant conflict of interests.
    XU Qinqi, PENG Jun, HE Chengqi, XIA Jingang, LIU Rui and HUANG Wei participated in the experimental design, paper preparation, and revision. All authors have read the final version of the paper and consented to its submission.
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