Selective Dissolution and Pore-Structure Modification of Dolostone Under Paired Temperature-Pressure Conditions: Insights from Continuous-Flow Acetic-Acid Experiments
Deep to ultra-deep dolostone reservoirs may be substantially modified by organic-acid-bearing fluids, but the relationship between fluid-phase chemical signals and residual pore-system modification under paired temperature–pressure (T–P) conditions remains insufficiently constrained. To address this gap, continuous-flo...