李峰峰,叶禹,余义常,郭睿

• 1:中国石油勘探开发研究院
• 2:中国石油集团工程技术研究院有限公司
• 3:中国石油国际勘探开发公司

摘要(Abstract)：

成岩作用是碳酸盐岩储层的重要成因之一，也是控制碳酸盐岩储层评价和预测的重要地质因素。首先概括了碳酸盐岩成岩研究的技术方法，重点剖析了溶蚀作用、白云石化作用、胶结作用、新生变形作用、硅化作用、压实作用和压溶作用的成岩机理及最新认识，归纳总结了生物扰动、构造破裂、烃类充注及微生物等成岩作用的辅助因素。碳酸盐岩成岩作用研究对象从礁滩和微生物岩逐步拓展到潟湖、混积岩及冷水沉积等领域。分析了构造-层序控制下成岩环境和成岩作用的演变，根据沉积能量和成岩性质划分出5种沉积环境-成岩作用组合。碳酸盐岩成岩作用研究存在问题包括：成岩模拟系统与真实地层环境差异大；成岩术语不规范、成岩模式理想化和单一化；潟湖、深水和冷水等非常规碳酸盐岩研究程度低；成岩作用的双刃性及对储层改造的定量化研究不足。指出了碳酸盐岩成岩作用研究的发展趋势：通过结合地层埋藏史，实验模拟方法将逐步趋向真实埋藏环境，成岩模拟软件不断实现模块集成化和智能化；成岩模式更加精细且更具针对性，成岩作用对储层的改造实现定量化研究；非常规碳酸盐岩成岩机理研究更加健全。

关键词(KeyWords)： 成岩作用;碳酸盐岩;溶蚀作用;白云石化作用;成岩模式

Abstract:

Keywords:

基金项目(Foundation): 中国石油科技重大专项(2021DJ3202;2022DJ3211)

作者(Author): 李峰峰,叶禹,余义常,郭睿

DOI: 10.19509/j.cnki.dzkq.2022.0209

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