Biomarker characteristics 0f source rock and bitumen and oil—source correlation of paleo—reservoir in northeastern Sichuan

  • XIONG Di ,
  • DING Xiaoqi ,
  • ZHU Zhiliang ,
  • LE Jinpeng
Expand
  • Biomarker characteristics 0f source rock and bitumen and oil—source correlation of paleo—reservoir in northeastern Sichuan

Online published: 2013-10-08

Abstract

Northeastern Sichuan is an important gas producing area of China,and its primary origin of gas is the cracking of crude oil of paleo-reservoir.On account of the uncertainty of oil sources of paleo—reservoir.the biomarker of reservoir bitumen of Changxing-Jialingjiang Formation and source rocks of Paleozonic and Mesozoic in northeastern Sichuan was analyzed and contrasted.The result shows that the organic matter of Lower Paleozonic source rocks was derived from hydrobios and algae;the organic matter of Upper Paleozonic source rocks was derived from a mixing source in which hydrobios and algae prevail over higher plants;the organic matter of Upper Paleozonic source rocks was dominated by higher plants.Paleozonic source rocks deposited in reducing to weakly reducing transitional environment with saline water and Mesozoic source rocks deposited in weakly reducing to weakly oxic transitional environment with flesh water. The main oil source formation of paleo—reservoir in Changxin Jialin iang Form~ion is Upper Permian Longtan Formation,

 

Cite this article

XIONG Di , DING Xiaoqi , ZHU Zhiliang , LE Jinpeng . Biomarker characteristics 0f source rock and bitumen and oil—source correlation of paleo—reservoir in northeastern Sichuan[J]. Lithologic Reservoirs, 2013 , 25(4) : 54 -62 . DOI: 10.3969/j.issn.1673-8926.2013.04.011

References

[1] 朱光有,张水昌,梁英波,等.四川盆地天然气特征及气源[J].地学前缘,2006,13(2):234-248.
[2] 马永生.四川盆地普光大气田的发现与勘探[J].海相油气地质,2006,11(2):35-40.
[3] 王一刚,窦立荣,文应初,等.四川盆地东北部三叠系飞仙关组高含硫气藏H2S 成因研究[J].地球化学,2002,31(6):517-524.
[4] 秦建中,付小东,刘效曾.四川盆地东北部气田海相碳酸盐岩储层固体沥青研究[J].地质学报,2007,81(8):1065-1071.
[5] 吴婷婷,王兴志,冯仁蔚.普光气田飞仙关组成岩作用对滩相储层的影响[J].岩性油气藏,2012,24(6):94-100.
[6] 杨家静,王一刚,王兰生,等.四川盆地东部长兴组—飞仙关组气藏地球化学特征及气源探讨[J].沉积学报,2002,20(2):349-353.
[7] 马永生,蔡勋育,李国雄.四川盆地普光大型气藏基本特征及成藏富集规律[J].地质学报,2005,79(6):858-865.
[8] 朱扬明,王积宝,郝芳,等.川东宣汉地区天然气地球化学特征及成因[J].地质科学,2008,43(3):518-532.
[9] Hao Fang,Guo Tonglou,Zhu Yangming,et al. Evidence for multiple stages of oil cracking and thermochemical sulfate reduction in the Puguang gas field,Sichuan basin,China[J]. AAPG Bulletin,2008,92(5):611-637.
[10] 蔡立国,饶丹,潘文蕾,等.川东北地区普光气田成藏模式研究[J].石油实验地质,2005,27(5):462-467.
[11] 马永生,蔡勋育,郭彤楼.四川盆地普光大型气田油气充注与富集成藏的主控因素[J].科学通报,2007,52(增刊Ⅰ):149-155.
[12] 秦建中,孟庆强,付小东.川东北地区海相碳酸盐岩三期成烃成藏过程[J].石油勘探与开发,2008,35(5):548-556.
[13] 李国军,郑荣才,唐玉林,等.川东北地区飞仙关组层序—岩相古地理特征[J].岩性油气藏,2007,19(4):64-70.
[14] 马永生,傅强,郭彤楼,等.川东北地区普光气田长兴—飞仙关气藏成藏模式与成藏过程[J].石油实验地质,2005,27(5):455-461.
[15] 马永生,郭旭升,郭彤楼,等.四川盆地普光大型气田的发现与勘探启示[J].地质论评,2005,51(4):477-480.
[16] 卢双舫,张敏.油气地球化学[M].北京:石油工业出版社,2008:206-213.
[17] 蒂索B P, 韦尔特D H,熊寿生,等.原油的组成、分类及地质因素对原油组成的影响[J].石油地质实验,1978,4:50-116.
[18] 彼得斯 K E,莫尔多万 J M.生物标记化合物指南———古代沉积物与石油中分子化石的解释[M].姜乃煌,张水昌,林永汉,等,译. 北京:石油工业出版社,1995:106-133,156-178.
[19] 曾宪章,梁狄刚,王忠然,等.中国陆相原油和生油岩中的生物标志物[M].兰州:甘肃科学技术出版社,1989:171-189.
[20] 梁狄刚,郭彤楼,陈建平,等.中国南方海相生烃成藏研究的若干新进展(二):南方四套区域性海相烃源岩的地球化学特征[J].海相油气地质,2009,14(1):1-15.
[21] 蒂索B P, 韦尔特D H.石油形成和分布[M].第2 版.徐永元,徐濂,郝石生,等,译.北京:石油工业出版社,1989:61-88.
[22] Hanson A D,Ritts B D,Zinniker D,et al. Upper Oligocene lacustrine source rocks and petroleum systems of the northern Qaidam basin,northwest China[J]. AAPG Bulletin,2001,85(4):601-619.
[23] 张立平,黄第藩,廖志勤.伽马蜡烷———水体分层的地球化学标志[J].沉积学报,1999,17(1):136-140.
[24] 陈中红,查明,金强.典型断陷湖盆C27三降藿烷参数演化及其控制因素———以东营凹陷古近系为例[J].沉积学报,2010,28(3):635-642.
[25] 傅家谟,盛国英.分子有机地球化学与古气候、古环境研究[J].第四纪研究,1992,12(4):306-320.
[26] Ten Haven H L,De Leeuw J W,Peakman T M,et al. Anomalies in steroid and hopanoid maturity indices [J]. Geochimica et Cosmochimica Acta,1986,50(5):853-855.
[27] 段毅,王智平,张辉,等.柴达木盆地原油烃类地球化学特征[J].石油实验地质,2004,26(4):359-364.
[28] 蔡勋育,韦宝东,赵培荣.南方海相烃源岩特征分析[J].天然气工业,2005,25(3):20-22.
[29] 王铜山,耿安松,孙永革,等.川东北飞仙关组储层固体沥青地球化学特征及其气源指示意义[J].沉积学报,2008,26(2):340-348.
Outlines

/