东北石油大学学报2024,Vol.48Issue(6) :17-30,48.DOI:10.3969/j.issn.2095-4107.2024.06.002

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 sec-ond member in Funing Formation in the Huazhuang Area,Gaoyou Sag,Subei Basin

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.48Issue(6) :17-30,48.DOI:10.3969/j.issn.2095-4107.2024.06.002

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 sec-ond member in Funing Formation in the Huazhuang Area,Gaoyou Sag,Subei Basin

陈洋 1尹楠鑫 1陈岑 1尤启东 2孔维军 3李立峰 3王馨玥 1赵娅 4曾强浩4
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作者信息

  • 1. 重庆科技大学石油与天然气工程学院,重庆 401331;重庆科技大学复杂油气田勘探开发重庆市重点实验室,重庆 401331
  • 2. 中国石化江苏油田分公司江苏油田开发部,江苏扬州 225009
  • 3. 中国石化江苏油田分公司江苏油田采油一厂,江苏扬州 225009
  • 4. 长江大学资源与环境学院,湖北武汉 403100
  • 折叠

摘要

苏北盆地高邮凹陷油气资源丰富,勘探开发潜力较高.以高邮凹陷花庄地区阜宁组二段(阜二段)典型页岩样品为研究对象,采用气相色谱—质谱联用(GC-MS)技术对生物标志化合物进行分析,采用X线衍射(XRD)法对黏土矿物进行定量测试,采用电感耦合等离子体质谱仪(ICP-MS)进行微量元素分析,明确有机质来源和沉积环境.结果表明:研究区有机质主要来源于低等水生生物,形成于还原环境.阜二段沉积早期以寒冷干旱的气候为主,降雨量较少;阜二段沉积后期降雨量逐渐增大,过渡到温暖湿润的气候.阜二段沉积早期水体环境为咸水环境,沉积后期水体咸度逐渐降低.潮湿条件下形成的湖泊是油页岩沉积的先决条件,缺氧还原环境与咸水沉积环境是有机质富集的关键因素.该结果对苏北盆地高邮凹陷花庄地区页岩油勘探具有指导意义.

Abstract

The Gaoyou Sag in the Subei Basin is rich in oil and gas resources,with high potential for ex-ploration 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 quantita-tive 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 re-sults 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 pre-dominantly cold and arid with low precipitation,transitioning to a warm and humid climate with increas-ing 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 con-ditions 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.

关键词

页岩油/有机质来源/古环境/陆相/阜宁组二段/古近系/花庄地区/高邮凹陷/苏北盆地

Key words

shale oil/organic matter source/paleoenvironment/continental facies/second member of Funing Formation/Paleogene/Huazhuang Area/Gaoyou Sag/Subei Basin

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出版年

2024
东北石油大学学报
东北石油大学

东北石油大学学报

CSTPCD北大核心
影响因子:1.274
ISSN:2095-4107
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