Reformation Mechanism of High-Quality Carbonate Reservoirs in Northeastern Sichuan Basin
详细信息   
摘要

The high-quality carbonate reservoirs in Puguang Gas Field of the northeastern Sichuan Basin are mainly dolomites of reef-bank facies. Secondary intragranular and intergranular pores work as the main reservoir spaces, accompanied with significant tectonic track ways. The secondary pores generated from 2 stages of dissolution during burial history. The 2 stages of tectonic movement (the early and the middle-late Yanshan movements) occurred at the same time as the 2 stages of dissolution, which gave birth to fractures and microfractures. Rock permeability was improved and acid fluids migrated into rocks. Non-selective dissolutions happened and “fracture-dissolved pore” combination formed.

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