摘要
油气储层的微观非均质性特征是储层地质学研究的重要内容之一。本文的目的是研究鄂尔多斯盆地镇北地区长3储层微观非均质性特征,研究方法是利用真实砂岩微观模型实验。通过实验发现鄂尔多斯盆地镇北地区长3和储层为致密型砂岩,真实砂岩微观模型实验直观地显示出鄂尔多斯盆地镇北地区长3储层具有很强的微观非均质性,砂岩的成岩作用和孔隙结构是影响本区长3储层微观非均质性的主要原因。在低渗透砂岩中,溶蚀作用引起砂岩产生强烈的非均质性,而这些砂岩则形成长3储层的高渗带。
The micro-anisotropy characteristics of the oil and gas reservoirs are one of the important contents in reservoir geology. Based on the authentic sandstone micro-model experiment, the micro-anisotropy characteristic of Chang 3 reservoirs of Zhenbei area in Ordos Basin was analyzed. Chang 3 reservoirs belong to tight sandstone. The authentic sandstone micro-model experiment audio-visually display the intense micro-anisotropy of Chang 3 reservoirs in this area. The sandstone pore structure and diagenesis are main factors influencing Chang 3 reservoirs micro-anisotropy. The dissolution resulted in the intense micro-anistropy of Chang 3 low permeable sandstone, but this sandstone formed high permeable zone of Chang 3 reservoirs in this area.
出处
《沉积学报》
CAS
CSCD
北大核心
2007年第2期224-229,共6页
Acta Sedimentologica Sinica
基金
国家973项目(编号:2003CB214607)
国家自然科学基金(批准号:40472099)
西北大学科研基金(编号:OKYQDF014)资助
关键词
微观非均质性
真实砂岩微观模型
实验分析
长3储层
镇北地区
鄂尔多斯盆地
micro-anisotropy, authentic sandstone micro-model, experimental analysis, Chang 3 reservoirs, Zhenbei area, Ordos Basin