收稿日期: 2011-04-15
修回日期: 2011-06-13
网络出版日期: 2011-10-10
基金资助
国家自然科学基金(编号:41103022);中科院西部之光人才培养西部博士项目(编号:Y134MF1ZMF);中国科学院油气资源研究重点实验室开放基金(编号:KFJJ2010-08)联合资助.
Geochemical Characteristics of Crude Oils from Wunan Oilfield,Qaidam Basin
Received date: 2011-04-15
Revised date: 2011-06-13
Online published: 2011-10-10
通过对柴达木盆地西南缘乌南油田原油样品饱和烃、芳烃生物标志化合物和单体烃碳同位素的系统分析,阐明了它们的地球化学特征。研究结果表明,样品中正构烷烃系列碳数分布具有双重性模式,Pr/Ph<0.5,呈强植烷优势;具有相对较高含量的三环萜烷和伽马蜡烷,藿烷C35/C34值基本上≤1;芳烃组分主要以萘系列、菲系列为主,三芳甾烷系列化合物含量较高,指示了乌南原油形成于半咸水—咸水湖相较强还原沉积环境,母质来源主要为低等水生生物,藿烷和甾烷成熟度参数反映其主要为低熟原油。原油单体烃碳同位素分布曲线模式整体上较为水平,高碳数略有增高的趋势,也表明了原油以水生生物和细菌为主的偏腐泥型有机质生源特征。
张明峰, 妥进才, 李中平, 刘立, 郭力军 . 柴达木盆地西南缘乌南油田原油地球化学特征[J]. 天然气地球科学, 2011 , 22(5) : 840 -847 . DOI: 10.11764/j.issn.1672-1926.2011.05.840
By measuring the stable carbon isotopes of satisfied hydrocarbon,aromatics and single hydrocarbons in crude oil collected from the Wunan oilfield in southwest margin of Qaidam basin,we discuss the geochemical features of the crude oil.The results indicate that the n-alkanes present a bimodal distribution pattern (i.e.,odd-to-even and even\|to\|odd carbon predominance),associated with low ratios of Pr/Ph (<0.5) and C35-Hopane/C34 -Hopane (<1.0),high abundance of tricyclic\|terpanes and gammacerane,and occurrence of hopane (C35).The aromatic hydrocarbons compounds were mainly composed of naphthalene and phenanthrene,and a relatively high amount of triaromatic steroid compounds occurs.These results confirm that the crude oils in the Wunan oilfield were formed in a mild\|salty to salty redution depositional environment,and the parent input matter mainly derived from the lower aquatic organisms.The biomarker parameters of thermal maturity (i.e.hopanes and steranes) suggest a low thermal maturity of the crude oil.Carbon isotope of crude oils (δ13C bulk) was relatively heavy,in contrast that the carbon isotope values of single molecule hydrocarbons (δ13C n-alkanes) remain unchanged with exception of carbon isotope increase in high carbon number,which also support that the source matter of crude oils were derived from aquatic organisms,as well as the sapropelic organic matter.
Key words: Qaidam basin; Wunan oilfield; Crude oil; Biomarker; Carbon isotope.
[1]Zhu Yangming,Su Aiguo,Liang Digang,et al.Geochemical characteristics and source rock age identification of crude oils in the Qaidam basin,northwest China[J].Acta Geologica Sinica,2003,77(2):272-279.[朱扬明,苏爱国,梁狄刚,等.柴达木盆地原油地球化学特征及其源岩时代判识[J].地质学报,2003,77(2):272-279.]
[2]Fowler M G,Abolins P,Douglas A G.Monocyclic alkanes in Ordovician organic matter[J].Organic Geochemistry,1986,10(4/6):815-823.
[3]Welte D H,Waples D W.ber die Bevorzugung geradzahliger n-alkane in sedimentgesteinen[J].Die Naturwissenschaften,1973,60(11):516-517.
[4]Damsté S,Ten Haven,Leeuw J W,et al.Restricted utility of the the pristine/phytane ratio as a palaeoenvironmental indicator[J].Nature,1987,330:641-643.
[5]Shi Yang,Bao Jianping,Zhu Cuishan,et al.Comparative study on geochemistry between crude oils from Qigequan and Xianshuiquan oilfields in western Qaidam basin[J].Natural Gas Geoscience,2010,21(1):132-138.[施洋,包建平,朱翠山,等.柴达木盆地西部七个泉与咸水泉油田原油地球化学特征对比研究[J].天然气地球科学,2010,21(1):132-138.]
[6]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.
[7]Duan Yi,Wang Zhiping,Zhang Hui,et al.Geochemical characteristics of hydrocarbons in crude oils from the Qaidam basin[J].Petroleum Geology & Experiment,2004,26(4):359-364.[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.]
[8]Volkman J K,Banks M R,Denwerk K,et al.Biomarker Composition and Depositional Setting Tasmanite Oil Shale from Northern Tasmania,Austrilia[C].Paris:14th International Meeting on Organic Geocehemistry,1989.
[9]Wang Tieguan.Geochemistry Research of Biomarkers[M].Wuhan:China University of Geosciences Press,1990:55-65.[王铁冠.生物标志物地球化学研究[M].武汉:中国地质大学出版社,1990:55-65.]
[10]Philp R P,Fan P,Lewis C A,et al.Geochemical characteristics of oils from Chaidamu,Shanganning and Jianghan basins,China[J].Journal of Southeast Asian Earth Science,1991,5(1/4):351-358.
[11]Ekweozor C M,Okogun J I,Ekong D E U,et al.C24—C27degraded triterpanes in Nigerian petroleum:Novel molecular markers of source/input or organic maturation[J].Journal of Geochemical Exploration,1981,15(1/3):653-662.
[12]Liu Yuhua,Wen Zhigang,Song Huanxin,et al.Geochemical characteristics and their signif icance of crude oils from Chang 3 oil layer group of Zhen 28 well field,Yanwu highland[J].Natural Gas Geoscience,2008,19(5):718-721.[刘玉华,文志刚,宋换新,等.鄂尔多斯盆地演武高地镇28井区长3油层组原油地球化学特征及其意义[J].天然气地球科学,2008,19(5):718-721.]
[13]Peters K E,Moldown J M.The Biomarker Guides:Interpreting Molecular Fossils in Petroleun and Ancient Sediments[M].New Jersey,USA:Prentice Hall,1993:111-120.
[14]Sinninghe Damsté J S,Kenig F,Koopmans M P,et al.Evidence for gammacerane as a indicator of water column stratification[J].Geochimicalet Cosmochimica Acta,1995,59(9):1895-1900.
[15]Tuo Jincai,Shao Hongshun,Huang Xingzhen.Lacustrine Carbonate source rocks and their organic geochemical characteristics:Taking the Tertiary system of Qaidam basin for example[J].Petroleum Geology & Experiment,1995,17(3):272-276.[妥进才,邵宏舜,黄杏珍.湖相碳酸盐岩生油岩及其有机地球化学特征——以柴达木盆地第三系为例[J].石油实验地质,1995,17(3):272-276.]
[16]Shi Yang,Bao Jianping,Zhu Cuishan,et al.Comparative study on geochemistry between crude oils from Qigequan and Xianshuiquan oilfields in western Qaidam basin[J].Natural Gas Geoscience,2010,21(1):132-138.[施洋,包建平,朱翠山,等.柴达木盆地西部七个泉与咸水泉油田原油地球化学特征对比研究[J].天然气地球科学,2010,21(1):132-138.]
[17]Seifert W K,Moldwan J M.Use of Biological Markers in Petroleum Exploration[M]// Johns R B.Methods in Geochemistry and Geophysics.Hardbound Elsevier,1986:261-290.
[18]Seifert W K,Moldowan J M.Application of steranes,terpanes and monoaromatics to the maturation,migration and source of crude oils[J].Geochimica et Cosmochimica Acta,1978,42 (1):77-95.
[19]Huang Difan,Li Jinchao,Zhang Dajiang,et al.Maturation sequence of Tertiary crude oils in the Qaidam basin and its significance in petroleum resource assessment[J].Journal of Southeast Asian Earth Sciences,1991,5(1/4):359-366.
[20]Li Zhenguang,Feng Zihui,Song Guixia,et al.Distribution and composition of aromatic hydrocarbons and classification of oil in Songliao basin[J].Oil & Gas Geology,2005,26(4):494-500.[李振广,冯子辉,宋桂侠,等.松辽盆地原油芳烃分布组成特征与原油类型划分[J].石油与天然气地质,2005,26(4):494-500.]
[21]Li Sumei,Zhang Aiyun,Wang Tieguan.Distribution pattern of pyrrolic nitrogen compound in crude oils[J].Oil & Gas Geology,2000,21(2):118-122.[李素梅,张爱云,王铁冠.原油中吡咯类含氮化合物的分布型式[J].石油与天然气地质,2000,21(2):118-122.]
[22]Li Shuifu,He Sheng.Geochemical characteristics of dibenzothiophene,dibenzofuran,and flurene and their homologues and their environmental indication[J].Geochimica,2008,37(1):45-50.[李水福,何生.原油芳烃中三芴系列化合物的环境指示作用[J].地球化学,2008,37(1):45-50.]
[23]Peters K E,Cunningham A E,Walters C C,et al.Petroleum systems in the Jiangling-Dangyang area,Jianghan basin,China[J].Organic Geochemistry,1996,24(10/11):1035-1060.
[24]Duan Yi,Zhang Hui,Wu Baoxiang,et al.Carbon isotopic studies of individual n-alkanes in crude oils from Qaidam basin[J].Journal of Mineralogy and Pettrology,2003,23(4):91-94.[段毅,张辉,吴保祥,等.柴达木盆地原油单体正构烷烃碳同位素研究[J].矿物岩石,2003,23(4):91-94.]
[25]Schouten S,Hartgers W A,Lòpez J F,et al.A molecular isotopic study of 13C-enriched organic matter in evaporitic deposits:Recognition of CO2-limited ecosystems[J].Organic Geochemistry,2011,32(2):277-286.
[26]Murray A P,Summons R E,Boreham C J,et al.Biomarker and n-alkane isotope profiles for Tertiary oils:Relationship to source rock depositional setting[J].Organic Geochemistry,1994,22 (3/5):521-542.
[27]Zhu Yangming,Su Aiguo,Liang Digang,et al.Geochemical characteristics of Tertiary saline lacustrine oils in the Qaidam basin[J].Chinese Journal of Geology,2004,39(4):475-485.[朱扬明,苏爱国,梁狄刚,等.柴达木盆地西部第三系咸水湖相原油地球化学特征[J].地质科学,2004,39(4):475-485.]
/
〈 |
|
〉 |