栾治盛,杜江峰,孙平昌,侯丽云,丁聪

• 1:吉林大学地球科学学院
• 2:吉林省油页岩及共生能源矿产重点实验室
• 3:中海油研究总院有限公司

摘要(Abstract)：

生烃热模拟实验是烃源岩成烃潜力与资源评价的重要手段,也是揭示页岩油气等非常规能源成藏序列的重要正演方法。生烃热模拟实验可以根据体系的开放性分为开放体系、封闭体系和半开放体系热模拟实验,选择不同的模拟实验方法应用于不同的研究目的。开放体系是与干酪根初始裂解反应最相近的热模拟方法,半开放体系是最为接近实际地质体中烃源岩热演化的热模拟体系,封闭体系更适用于Ⅲ型干酪根生烃模拟的研究,是认识重烃二次裂解的重要方法。在有机质热演化过程中,生成油气会受温度、压力、水介质、催化剂等条件的影响,这些外界因素也会对热模拟实验产生重要影响。热模拟实验在非常规资源中应用较广泛,既可以研究烃源岩的生排烃特征、成烃潜力及油气滞留特征;也可以分析作为储层的泥页岩的储集物性及孔隙类型演化特征等。目前热模拟实验在碳酸盐岩烃源岩热模拟实验、页岩热演化过程中的微米-纳米孔隙结构变化特征,有机质生排烃与泥页岩储集物性的协同演化关系这三个方面取得重要进展,也是未来的主攻方向。

关键词(KeyWords)： 热模拟;有机质;储层;非常规油气;发展方向

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金项目“松辽盆地上白垩统青山口组有机质旋回的天文年代信息示踪及有机质富集定量模型建立”(41402088);国家自然科学基金项目“油页岩纹层中古环境信息重建及毫米级有机质富集机理研究”(41772092)和松辽盆地基底古生界油气潜力评价(DD20211341)

作者(Author): 栾治盛,杜江峰,孙平昌,侯丽云,丁聪

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