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深部碎屑岩储层次生孔隙发育机理研究进展

The New Advances of Secondary Porosity Genesis Mechanism in Deep Clastic Reservoir

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【作者】 黄洁朱如凯侯读杰阮伟

【Author】 HUANG Jie1,ZHU Ru-kai2,HOU Du-jie1,RUAN Wei1(1.School of Energy Resources,China University of Geosciences,Beijing 100083,China;2.Research Institute of Petroleum Exploration and Development,CNPC,Beijing 100083,China)

【机构】 中国地质大学能源学院中国石油天然气股份有限公司勘探开发研究院中国地质大学能源学院 北京100083北京100083

【摘要】 从深部碎屑岩储层次生孔隙的溶蚀机理、溶蚀矿物的种类、影响因素3个方面总结了近年来深部储层次生孔隙的研究成果。深部储层次生孔隙的发育受众多因素影响,异常高压、断裂发育、深部热流体活动、流体交换等都会对次生孔隙的发育产生有益的影响。提出了应该重视深部与中浅层物理化学性质的差别,综合系统地研究深部碎屑岩储层次生孔隙的成因与分布,特别是模拟高温高压条件下矿物溶蚀和沉淀的机理及其影响因素,全面突破深部储层次生孔隙理论,指导勘探开发。

【Abstract】 Porosities,both primary and secondary,are the important places to reserve oil and gas.At present,the study in the genesis and distribution of clastic reservoir porosity almost concentrates on shallow and mid-depth zones.With deep oil and gas being discovered and developed,the mechanism and forecast of secondary porosity in deep zones becomes especially important.This paper,from the corrosion mechanism,variety of corroded minerals and corrosion influence factors,summarizes the advances in deep-reservoir secondary porosity during latest years.It is found that the generation of deep-reservoir secondary porosity can be promoted by many factors,such as abnormal pressure,fracture systems,deep-hot fluids and exchange of fluids.Importance should be attached to the difference in physics and chemistry between shallow and deep reservoirs in order to make breakthroughs in the exploration and development.Also,every factor should be thought about synthetically and systemically.In addition,the erosion and precipitation of minerals especially needs to be simulated in high temperature and high pressure.

【基金】 中国石油天然气股份有限公司“十一五”重点科技攻关项目(06-01C-01);中国地质大学(北京)沉积盆地能源地质实验室基金项目
  • 【文献出处】 地质科技情报 ,Geological Science and Technology Information , 编辑部邮箱 ,2007年06期
  • 【分类号】P618.13
  • 【被引频次】111
  • 【下载频次】1006
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