陆相页岩油有机质来源与沉积环境分析——以苏北盆地高邮凹陷花庄地区古近系阜宁组二段为例
陈洋 , 尹楠鑫 , 陈岑 , 尤启东 , 孔维军 , 李立峰 , 王馨玥 , 赵娅 , 曾强浩
东北石油大学学报 ›› 2024, Vol. 48 ›› Issue (6) : 17 -30.
陆相页岩油有机质来源与沉积环境分析——以苏北盆地高邮凹陷花庄地区古近系阜宁组二段为例
Organic matter sources and depositional environment analysis of continental shale oil : a case study of Paleogene second member in Funing Formation in the Huazhuang Area, Gaoyou Sag, Subei Basin
The Gaoyou Sag in the Subei Basin is rich in oil and gas resources, with high potential for exploration and development. This study focuses on typical shale samples from the second member of the Funing Formation (E1f2) in the Huazhuang Area of the Gaoyou Sag. Gas chromatography-mass spec-trometry(GC-MS) was used to analyze biomarkers, X-ray diffraction(XRD) was employed for quantitative analysis of clay minerals, and inductively coupled plasma mass spectrometry(ICP-MS) was applied for trace element analysis to determine the organic matter sources and depositional environment. The results indicate that the organic matter in the study area primarily originated from lower aquatic organisms and was deposited in a reducing environment. During the early deposition of E1f2, the climate was predominantly cold and arid with low precipitation, transitioning to a warm and humid climate with increasing rainfall in the later stage. The early depositional environment was characterized by saline water, while salinity gradually decreased in the later stage. The formation of lakes under humid conditions was a prerequisite for oil shale deposition, while an anoxic reducing environment and saline depositional conditions were critical for organic matter enrichment. These findings provide valuable guidance for shale oil exploration in the Huazhuang Area of the Gaoyou Sag in the Subei Basin.
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重庆市自然科学基金项目(cstc2020jcyj-msxmX0869)
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