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鄂尔多斯盆地北部古岩溶储层流体-岩石系统孔隙发育规律及成岩圈闭定量预测
引用本文:王英民,曹正,赵锡奎.鄂尔多斯盆地北部古岩溶储层流体-岩石系统孔隙发育规律及成岩圈闭定量预测[J].矿物岩石,2003,23(3):51-56.
作者姓名:王英民  曹正  赵锡奎
作者单位:1. 石油与天然气成藏机理教育部重点实验室,北京,102249;石油大学(北京)盆地与油藏研究中心,北京,102249
2. 中国石油勘探开发研究院西北分院,甘肃,兰州,730020
3. 成都理工大学能源学院,四川,成都,610059
基金项目: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"(G1999043305)
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。

关 键 词:鄂尔多斯盆地  化学动力学  化学热力学  流体动力学  古岩溶储层  承压流  潜流  流体-岩石系统  成岩圈闭  定量预测  油气勘探
文章编号:1001-6872(2003)03-0055-06
修稿时间:2003年4月22日

QUANTITATIVE STUDY OF PORE DEVELOPMENT AND FILLING ZONE IN THE FLUID-ROCK SYSTEM ON THE FOSSIL KARST RESERVOIR IN THE NORTH OF ORDOS BASIN,CHINA
WANG Ying-min.QUANTITATIVE STUDY OF PORE DEVELOPMENT AND FILLING ZONE IN THE FLUID-ROCK SYSTEM ON THE FOSSIL KARST RESERVOIR IN THE NORTH OF ORDOS BASIN,CHINA[J].Journal of Mineralogy and Petrology,2003,23(3):51-56.
Authors:WANG Ying-min
Institution:WANG Ying-min~
Abstract: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.
Keywords:chemical kinetics and thermodynamics  hydrodynamics  fossil karst reservoir  underwater current water model  bearing current water model  fluid-rock system  diagenesis trap
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