龙门山北段山前带侏罗系油砂岩成因研究

戴鸿鸣; 刘文龙; 杨跃明; 李跃纲; 段勇

doi:10.11781/sysydz200706604

龙门山北段山前带侏罗系油砂岩成因研究

doi: 10.11781/sysydz200706604

1.
西南石油大学, 成都 610500
2. 中国石油西南油气田分公司川西北气矿, 四川江油 621700

基金项目: 四川省高校重点实验室项目(2006ZD044)

详细信息

作者简介:
戴鸿鸣(1963- ),男(汉族),重庆长寿人,副教授,从事油气地质和油气地球化学的研究和教学工作.

中图分类号: TE122.1
计量
- 文章访问数: 882
- HTML全文浏览量: 94
- PDF下载量: 484
- 被引次数: 0
出版历程
- 收稿日期: 2006-11-01
- 修回日期: 2007-10-23
- 刊出日期: 2007-11-28

THE ORIGIN OF JURASSIC OIL-SOAKED SANDSTONE IN THE PIEDMONT ZONE OF NORTH LONGMENSHAN, THE SICHUAN BASIN

1.
Southwest Petroleum University, Chengdu, Sichuan 610500, China
2. Northwest Sichuan Gas Field Mine, Southwest Oil and Gas Field Brand, PetroChina, Jiangyou, Sichuan 621700, China

摘要

摘要: 龙门山北段山前带处于推覆体构造带的断层隐伏前锋构造带,已发现中坝、河湾场气田和较多油气显示。野外调查和钻井发现侏罗系油浸砂岩广泛存在,认为油砂岩中原油是寒武系泥质烃源岩在生油高峰期生成的原油经历了不同程度的生物降解和长距离的运移后,在多期构造幕作用下,多次充注、运移、再分配的产物。主要依据为:油砂岩正构烷烃和支链烷烃均已消失,遭受强烈生物降解;芳烃碳同位素相近,为-34.41‰~-35.03‰;裂解产物轻烃正构烷烃相对支链烷烃占优势,属海相Ⅰ—Ⅱ₁干酪根生成产物;生物标志化合物分布特征与寒武系黑色泥岩相似;甲基菲指数折算的成熟度为0.82%~1.25%。
- 油气地球化学 /
- 油砂岩 /
- 侏罗系 /
- 龙门山北段 /
- 四川盆地
Abstract: The piedmont zone of the North Longmenshan is located at the fault front structural zone of buried faults of the nappe structural belt.Zhongba and Hewangchang Gasfeilds and more hydrocarbon show are discovered.The Jurassic oil-soaked sandstone is discovered to be wide distribution by field survey and well drilling.It believes that the crude oil of oil-soaked sandstone is the product which generates in the oil generation peak of Cambrian muddy source rock.It is the production by more time charging,movement and redistribution,which is after the varying degrees biodegradation and long distance movement,and under the polytectonic movement.The main criterions are following.First,the normal alkane and branched paraffin of oil-soaked sandstone disappear by strong biodegradation.Second,the carbon isotope of aromatic hydrocarbon is Closed.It is-34.41‰～-35.03‰.Light hydrocarbon normal alkane in the hydrolytic product is predominantly to compare with hydrocarbon branched paraffin.It belongs to the product of marine Ⅰ-Ⅱ₁ type kerogen.Third,the pattern of biomarker is similar to Cambrian dark Claystone.At last,the maturity which is converted by methylphenanthrene index is 0.82%～1.25%.
- hydrocarbon geochemistry /
- oil-soaked sandstone /
- Jurassic the North Longmenshan /
- the Sichuan Basin /

HTML全文

参考文献(14)

[1]	宋文海.论龙门山北段推覆构造及其油气前景[J].天然气工业,1989,19(3):2～9
[2]	何鲤,刘莉萍,罗潇等.川西龙门山推覆构造特征及有利油气勘探区块预测[J].石油实验地质,2007,29(3):247～252
[3]	王兰生,韩克猷,谢邦华等.龙门山推覆构造带北段油气田形成条件探讨[J].天然气工业,2005,25(S1):1～5
[4]	张林,魏国齐.四川盆地震旦系-下古生界沥青产烃潜力及分布特征[J].石油实验地质,2005,27(3):276～280
[5]	徐世琦,曾庆,唐大海等.江油厚坝油砂岩成藏条件分析[J].天然气勘探与开发,2005,28(3):1～4
[6]	刘云生,郭战峰,梁西文等.中上扬子地区晚三叠世-侏罗纪砂岩构造意义及盆山耦合关系[J].石油实验地质,2006,28(3):201～205
[7]	胡晓强,陈洪德.川西前陆盆地侏罗系三角洲沉积体系与沉积模式[J].石油实验地质,2005,27(3):226～231
[8]	Stahl W J.Compositional changes and ¹³C/12C fractionations during the degradation of hydrocarbons by bacteria[J].Geochimica et Cosmochimica Acta,1980,44:1903～1907
[9]	Leytaeuser D A.Generation and migration of C₂-C₇ light hydrocarbons in sedimentary basin[J].Org Geochem.,1979,1:119～124
[10]	戴金星,裴锡古,戚厚发.中国天然气地质学(卷一)[M].北京:石油工业出版社,1992.75～76
[11]	Thompson K F M.Light hydrocarbons in subsurface sediments[J].Geochim et Cosmochim Acta,1979,43:657～672
[12]	Thompson K F M.Classification and thermal histroy of petroleum based on light hydrocarbons[J].Geochim et Cosmochim Acta,1983,47:307～316
[13]	谢邦华,王兰生,张鉴等.龙门山北段烃源岩纵向分布及地化特征[J].天然气工业,2003,23(5):21～23
[14]	陈昭国.四川盆地川西坳陷深盆气探讨[J].石油实验地质,2005,27(1):32～38