岩性油气藏 ›› 2015, Vol. 27 ›› Issue (1): 1–13.doi: 10.3969/j.issn.1673-8926.2015.01.001

• 讨论与争鸣 •    下一篇

致密砂岩气储层的沉积-成岩成因机理探讨与热点问题

于兴河,李顺利,杨志浩   

  1. 中国地质大学(北京),北京 100083
  • 出版日期:2015-02-03 发布日期:2015-02-03
  • 第一作者:于兴河( 1958- ),男,博士,教授、博士生导师,主要从事沉积学、储层表征建模及油气地质方面的研究和教学工作。 地址:( 100083 )北京市海淀区学院路 29 号中国地质大学(北京)能源学院。 E-mail: billyu@cugb.edu.cn 。
  • 基金资助:
    教育部博士点基金项目沉积盆地斜坡带河流三角洲沉积作用多样性及其储层构型与非均质响应机理(编号: 20120022130002 )和国家自然科学基金项目砾岩结构 - 成因分类、沉积成岩机理及其岩石物性响应模型(编号: 41472091 )联合资助

Discussion on deposition-diagenesis genetic mechanism and hot issues of tight sandstone gas reservoir

YU Xinghe,LI Shunli,YANG Zhihao   

  1. China University of Geosciences , Beijing 100083 , China
  • Online:2015-02-03 Published:2015-02-03

摘要: 致密砂岩气与页岩气是当前非常规天然气中的两大主力勘探领域,均为今后 10~20 年接替常规油气资源的重要来源。 无论从对其地质规律的认识,还是从其勘探开发的技术上讲,在未来 10 年里致密砂岩气比页岩气更为现实。 然而,有利储集空间的准确预测已成为当前致密砂岩油气勘探与开发的主要瓶颈,而解决这一问题的核心就是要首先厘清其储层的沉积与成岩成因。 从我国典型致密砂岩气田的研究与国外资料的分析可以发现,其沉积时通常具有水动力弱而稳定、沉积速率相对较为缓慢、多为过渡相环境或三角洲沉积产物的特征,多发育在与煤系有关的(薄互层)地层之中,这些因素是形成致密砂岩的必要条件;早成岩期的持续压实是其致密最主要的过程,而盆地的多旋回构造运动所造成的低地温梯度下的复杂埋藏史是促使其致密的充分条件。 因而,多旋回的前新生界低温沉积盆地中的异常压力区通常是寻找致密砂岩气的有利区域,而三角洲前缘的薄互层含煤层系砂岩则是其主要的勘探开发层位。 在储层寻找与评价上应重视致密砂岩储层的非均质特点, 大力研究其微观孔隙结构变化对渗透率的影响,应用渗透率盲区与异常压力数据来辅助评价其产层的优劣,并依此观点提出了我国致密砂岩气今后加强研究与勘探开发的六大战略选区。

Abstract: Tight sandstone gas and shale gas are currently two major unconventional hydrocarbon resources, which will be the significant resources for replacing the conventional oil and gas in next 10 to 20 years. Despite the understanding of geological property, or the technology of exploration and development, tight sandstone gas will be easily realized than shale gas in the next 10 years. However, precise prediction of favorable reservoir space has become a bottleneck for current tight sandstone gas exploration and development. Clarifying the deposition-diagenesis genetic mechanism of tight sandstone reservoir is the key to solve this problem. According to the research on the typical tight sandstone gas fields in China and data analysis abroad, tight sandstone generally deposited under weak hydrodynamic stability and relatively low depositional rate that much developed in coal-bearing(thin bed interbedded) strata of the transitional environments or deltas. Hence, these depositional mechanisms facilitate the requirement of forming tight sandstone. Continuous compaction during early diagenetic stage is the main process for their tight nature. The complex burial history under low geothermal gradients which were caused by multi-cycle movements of basin is the sufficient condition for forming tight sandstone reservoirs. Therefore, abnormal pressure zones in multi-cycle pre-Tertiary basins with low geothermal are the favorable area for exploring tight sandstone gas. The sandstones with thin interbedded coal-bearing strata in delta front are primary exploration and development intervals. Heterogeneity characteristics of tight sandstone play an important role on reservoir exploring and evaluating. The effect of microscopic pore structure change on permeability should be studied for evaluating pay reservoirs property. “Permeability blind area” and abnormal pressure data were employed for evaluating quality of reservoir. On the basis of this idea, we proposed six prospective areas for tight sandstone exploration and development in China in future.

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