The Main Controlling Factors of the Cambrian Ultra-Deep Dolomite Reservoir in the Tarim Basin
Abstract
:1. Introduction
2. Geological Setting
3. Distribution Characteristics of Porosity and Permeability
3.1. Series2
3.2. Miaolingian
3.3. Furongian
4. Main Controlling Factors of Favorable Reservoirs in the Tarim Basin
4.1. Unconventional Reservoirs
4.2. Main Controlling Factors for Conventional Reservoir
4.2.1. Controlling Factors during the Deposition Stage of Dolomite Reservoirs
- Tectonism
- 2.
- Sedimentary environment
- 3.
- Microorganism
4.2.2. Controlling Factors during the Diagenetic Stage of Dolomite Reservoirs
- Diagenesis
- 2.
- Structure and fracture development
- 3.
- Dissolution and filling effect
5. Conclusions
Author Contributions
Funding
Data Availability Statement
Acknowledgments
Conflicts of Interest
References
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Zhang, K.; You, X.; Ma, T.; Wang, J.; Wu, Y.; Lu, Y.; Zhang, S. The Main Controlling Factors of the Cambrian Ultra-Deep Dolomite Reservoir in the Tarim Basin. Minerals 2024, 14, 775. https://doi.org/10.3390/min14080775
Zhang K, You X, Ma T, Wang J, Wu Y, Lu Y, Zhang S. The Main Controlling Factors of the Cambrian Ultra-Deep Dolomite Reservoir in the Tarim Basin. Minerals. 2024; 14(8):775. https://doi.org/10.3390/min14080775
Chicago/Turabian StyleZhang, Kehui, Xuelian You, Tianyi Ma, Jia Wang, Yifen Wu, Yi Lu, and Shaoqi Zhang. 2024. "The Main Controlling Factors of the Cambrian Ultra-Deep Dolomite Reservoir in the Tarim Basin" Minerals 14, no. 8: 775. https://doi.org/10.3390/min14080775