Mesogenetic diagenesis of the Ordovician limestone in Yubei area, Tarim Basin, NW China

@article{Bai2020MesogeneticDO,
  title={Mesogenetic diagenesis of the Ordovician limestone in Yubei area, Tarim Basin, NW China},
  author={H. Bai and Wenhui Huang and Feng Wu and Benjun Ma and Weiqi Wang},
  journal={Carbonates and Evaporites},
  year={2020},
  volume={35},
  pages={1-18}
}
The Lower Ordovician succession, consisting of the Yingshan and Penglaiba formations, encompasses significant petroleum reservoirs in Yubei area, southwest Tarim Basin. Mesogenetic dissolution and dolomitization strongly contributed to the increase in rock porosities here. Wells YB 7, YB 5, and YB 1-2X drilled in eastern Yubei area met the deposits of Yingshan and Penglaiba formations, providing abundant data for the mesogenetic diagenesis analysis. Among them, Well YB 5 encountered the… Expand

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