Reservoir Geological Model of Reef-Bank Carbonate Rocks of Ordavician in Tazhong Area, Tarim Basin, NW China

Abstract:

The reservoir of Lianglitage formaton mainly distribute in the Liang 1~Liang 2 section, and slight amount distribute in Liang 3 section. The microfacies are abundant and, and they apparently affect the development of the reservoir. Based on the geologic feature, we propound the concept:"microfacies combination". It is composed by two or several microfacies, and each microfacies have similar reservoir conditions. Using the seismic facies interpretation, combining the methods of deterministic modeling and stochastic modeling, the "microfacies combination" model is established. Appling the method that "microfacies combination" controls the modeling course, taking the wave impedance which has good corresponding relationship with reservoir as secondary variable, small layer application of stochastic modeling method based on the porosity model is finally established through the stochastic modeling method layer and layer. Considering the crack influence on permeability, the first step is establishing the fracture distribution model, then the permeability model is established taking the fracture distribution as secondary variable, which improves the practicability of permeability model.

• Periodical: Advanced Materials Research (Volumes 765-767)
• Pages: 2949-2951
• DOI: https://doi.org/10.4028/www.scientific.net/AMR.765-767.2949
• Online since: September 2013
• Authors: Hai Zhou Qu, Zhen Yu Wang, Xi Wang, Kun Yu Fan, Yun Feng Zhang
• Keywords: Carbonate Rocks, Microfacies Combination, Ordovician, Reef-Bank Facies, Reservoir Model, Tarim Basin, Tazhong Area

References

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