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柴达木盆地尕斯库勒油田原油饱和烃地球化学特征及成因研究
引用本文:莫晓靥,张敏,张俊. 柴达木盆地尕斯库勒油田原油饱和烃地球化学特征及成因研究[J]. 天然气地球科学, 2011, 22(5): 848-853. DOI: 10.11764/j.issn.1672-1926.2011.05.848
作者姓名:莫晓靥  张敏  张俊
作者单位:1.长江大学地球化学系,湖北 荆州 434023;
2.长江大学油气资源与勘探技术教育部重点实验室,湖北 荆州 434023;
3.中国石油化工股份有限公司科技部,北京 100728
基金项目:国家自然科学基金项目(编号:40973041)资助
摘    要:尕斯库勒油田是柴达木盆地最大的油田,通过GC|MS分析技术,系统剖析了尕斯库勒油田原油的地球化学特征。研究结果表明:正构烷烃呈偶奇优势,其中浅部油藏中有部分原油正构烷烃缺乏,遭受到轻度的生物降解。对于正常原油,均具有较低的姥植比,同时具有含量丰富的伽马蜡烷和C35升藿烷,揭示了原油形成于强还原咸水环境,对比深部E13油藏和浅部N1-N12油藏,浅部油藏的成油环境的古盐度略低于深部油藏;原油中C21-/C22+值在1.02~1.71之间,且具有高含量的C27甾烷,指示了其母质来源以菌藻类低等水生生物为主;原油中C29αββ/(αββ+ααα)值以及Ts/Tm值都较低,都表现出了低熟油的特征,同时C2920S/(20S+20R)值普遍偏低,在深部E13油藏该值分布在0.31~0.40之间,而在浅部N1-N12油藏该值相对较低,分布在0.29~0.36之间,深部油藏的成熟度略高于浅部油藏。

关 键 词:柴达木盆地  尕斯库勒油田  原油  饱和烃  地球化学特征  
收稿时间:2010-04-01

Geochemical Characteristics of Saturated Hydrocarbon and Its Genesis in Hure Oilfield of Western Qaidam Basin
MO Xiao-ye,,ZHANG Min,ZHANG Jun. Geochemical Characteristics of Saturated Hydrocarbon and Its Genesis in Hure Oilfield of Western Qaidam Basin[J]. Natural Gas Geoscience, 2011, 22(5): 848-853. DOI: 10.11764/j.issn.1672-1926.2011.05.848
Authors:MO Xiao-ye    ZHANG Min  ZHANG Jun
Affiliation:1.Department of Geochemistry,Yangtze University,Jingzhou 434023,China;
2.Key Laboratory of Exploration Technologies for Oil and Gas Resoureces,Ministry of Education,
Yangtze University,Jingzhou 434023,China;3.Department of Technology,SINOPEC,Beijing 100728,China
Abstract:Hure oilfield is the biggest oil field in the Qaidam basin.In this paper,we comprehensively integrate the geochemical characteristics of saturated hydrocarbon by means of GC-MS analysis.The results show that the crude oil has even-odd carbon predominance for n-alkanes,where biogenicdegradation of crude oil in the shallow reservoir caused the absence of part of n-alkane serials.The normal oil has low Pr/Ph ratios,abundance of gammacerane and C35 homohopane,indicating that the crude oil was formed in strongly...
Keywords:Qaidam basin  Hure oilfield  Crude oil  Saturated hydrocarbon  Geochemical characteristic.  
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