摘要
在化学动力学及热力学、流体动力学和弥散动力学等理论的基础上 ,建立古岩溶储层岩溶斜坡地质模型和数学模型 ,对模型的承压流、潜流模式流体岩石系统进行动力学模拟研究 ,得出岩溶斜坡剖面上孔隙发育带和孔隙充填带的有利区 ,并探讨形成成岩圈闭的形成机理、模式和有利部位。
The chemical kinetics,thermodynamics, hydrodynamics,were used to establish the geological models and mathematical coupling model of fluid-rock system of karst ramp of fossil karst reservoir, and the fluid-rock system of underwater current model and bearing current model were simulated dynamiccally by computer.Then the advantageous areas of pore developing zone or filling zone on the section of fossil karst reservoir were obtained.The formation mechanism of diagenesis trap,model and favourable position were discussed.
出处
《矿物岩石》
CAS
CSCD
北大核心
2003年第3期51-56,共6页
Mineralogy and Petrology
基金
国家重点基础研究发展规划课题"中国典型叠合盆地应力场分析与构造变形三维解析" (G19990 43 3 0 5 )
