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陆相沉积盆地有机质的热演化是其在地质-地化作用下形成石油的重要机理。对沉积物中有机质热演化特性的了解是分析石油形成机理的重要基础。热分析样品预处理简单，实验时间短，研究已经证明热分析是表征有机质的简单、快速，并且可靠的分析技术[1]。
湖泊沉积物柱芯有机质厌氧热解行为垂直分布特征
【摘 要】
：
陆相沉积盆地有机质的热演化是其在地质-地化作用下形成石油的重要机理。对沉积物中有机质热演化特性的了解是分析石油形成机理的重要基础。热分析样品预处理简单，实验时
【机 构】
：
中国环境科学研究院,环境基准与风险评估国家重点实验室,北京100012
【出 处】
：
中国化学会第六届全国热分析动力学与热动力学学术会议
【发表日期】
：
2017年11期
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