桦甸盆地始新统油页岩岩石地球化学特征及富集规律研究
摘要
本文以东北地区有代表性的“小而肥”的新生代小型断陷含油页岩盆地——桦甸盆地为靶区,在大量测试数据分析基础上,详细研究油页岩的岩石矿物学、有机地球化学和元素地球化学特征。
运用盆地分析方法和层序地层学理论,开展桦甸盆地沉积构造演化特征综合研究,对盆地的构造演化、地层时代、层序格架、沉积相展布特征进行整体分析；首次采用共存因子分析的方法对桦甸盆地始新世中晚期古气候进行定量重建；在统一层序格架内,揭示了构造和气候条件对断陷盆地油页岩成矿的重要控制作用。
从定性恢复和半定量计算角度,首次估算了桦甸盆地桦甸组时期古湖泊生产力。从油页岩的有机质来源及保存条件研究入手,揭示了油页岩中有机质的富集机制,建立了陆相淡水-半咸水断陷盆地油页岩成矿模式。
运用盆地分析方法和层序地层学理论,开展桦甸盆地沉积构造演化特征综合研究,对盆地的构造演化、地层时代、层序格架、沉积相展布特征进行整体分析；首次采用共存因子分析的方法对桦甸盆地始新世中晚期古气候进行定量重建；在统一层序格架内,揭示了构造和气候条件对断陷盆地油页岩成矿的重要控制作用。
从定性恢复和半定量计算角度,首次估算了桦甸盆地桦甸组时期古湖泊生产力。从油页岩的有机质来源及保存条件研究入手,揭示了油页岩中有机质的富集机制,建立了陆相淡水-半咸水断陷盆地油页岩成矿模式。
引文
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