Hydrothermal dissolution of Ordovician carbonates rocks and its dissolution mechanism in Tarim Basin, China

@article{Liu2016HydrothermalDO,
  title={Hydrothermal dissolution of Ordovician carbonates rocks and its dissolution mechanism in Tarim Basin, China},
  author={L. Liu and Y. Ma and Bei Liu and C. Wang},
  journal={Carbonates and Evaporites},
  year={2016},
  volume={32},
  pages={525-537}
}
The dissolution of carbonate rocks has a significant control on reservoir quality under deep burial conditions, which has become a focus of studies in recent years. A series of hydrothermal minerals and combinations, such as fluorite, dickite, barite and hydrothermal dolomite, were discovered in the Ordovician strata in some exploration wells in the Tahe area. Moreover, the analysis results of carbon and oxygen isotope, REE, strontium isotope and inclusion homogenization temperature further… Expand
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References

SHOWING 1-10 OF 51 REFERENCES
Effects of Deep Fluid on Carbonates Reservoir in Tarim Basin
Transforming Effect of Deep Fluids on Carbonate Reservoirs in the Well TZ45 Region
Scientific research frontiers and considerable questions of carbonate diagenesis
Differences between fluid activities in the Central and North Tarim Basin
...
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