塔里木盆地塔中隆起寒武系深层油气地球化学特征及成因

doi:10.11743/ogg20170210

石油与天然气地质 ›› 2017, Vol. 38 ›› Issue (2): 302-310.doi: 10.11743/ogg20170210

塔里木盆地塔中隆起寒武系深层油气地球化学特征及成因

史江龙^1,2,3, 李剑^2,3, 李志生^2,3, 郝爱胜^2,3

1. 中国科学院大学渗流流体力学研究所, 河北廊坊 065007;
2. 中国石油勘探开发研究院廊坊分院, 河北廊坊 065007;
3. 中国石油天然气集团公司天然气成藏与开发重点实验室, 河北廊坊 065007

收稿日期:2016-09-20 修回日期:2017-02-20 出版日期:2017-04-28 发布日期:2017-05-04
通讯作者: 李剑(1966-),男,教授,天然气地球化学、天然气成藏、天然气资源评价。E-mail:lijian69@petrochina.com.cn。 E-mail:lijian69@petrochina.com.cn
第一作者简介:史江龙(1989-),男,硕士研究生,油气地质地球化学。E-mail:shijl5118@163.com。
基金项目:
国家科技重大专项（2011ZX05007）。

Geochemical characteristics and origin of the deep Cambrian oil and gas in the Tazhong Uplift,Tarim Basin

Shi Jianglong^1,2,3, Li Jian^2,3, Li Zhisheng^2,3, Hao Aisheng^2,3

1. Institute of Porous Flow Fluid Mechanics, University of Chinese Academy of Sciences, Langfang, Heibei 065007, China;;
2. Research Institute of Petroleum Exploration and Development-Langfang, PetroChina, Langfang, Heibei 065007, China;;
3. The Key Laboratory of Gas Reservoir Formation and Development, CNPC, Langfang, Heibei 065007, China

Received:2016-09-20 Revised:2017-02-20 Online:2017-04-28 Published:2017-05-04

摘要/Abstract

摘要： 塔中隆起寒武系碳酸盐岩储层油气资源丰富，然而由于复杂的构造地质背景，油气来源和天然气类型还存在较大争议。通过详细分析ZS1井、ZS1C井和ZS5井寒武系不同层段中凝析油和天然气的组成、碳同位素等特征，并结合寒武系-下奥陶统与中、上奥陶统烃源岩地球化学特征，对其油气来源和天然气成因类型进行了判别。研究结果表明，该区天然气为典型的腐泥型干酪根裂解气，其中寒武系肖尔布拉克组天然气干燥系数大于0.98，N₂含量介于2.5%~4.0%，为过成熟干气，且凝析油族组分与和饱和烃单体烃碳同位素偏重，nC₉-nC₂₀碳同位素介于-28.8‰~-26.3‰，表明油气来源为寒武系-下奥陶统烃源岩。而寒武系阿瓦塔格组和吾松格尔组天然气干燥系数介于0.63~0.78，N₂含量介于0.2%~0.8%，为低成熟湿气，且凝析油族组分和饱和烃单体烃碳同位素相对较轻，nC₉-nC₂₃碳同位素介于-37.25‰~-32.56‰，表明油气来源为中、上奥陶统烃源岩。

关键词: 天然气类型, 油气源, 有机地球化学, 寒武系, 塔中隆起, 塔里木盆地

Abstract: The Cambrian carbonate reservoirs of Tazhong uplift is rich in oil and gas.However,there are different opinions on the origin and genetic types of oil and gas in this area due to the complex tectonic setting.In this paper,we studied the origin and genetic types of oil and gas through a detailed analysis of the composition and carbon isotope data of condensate oil and gas in different intervals of the Cambrian in ZS1,ZS1C and ZS5 wells and the geochemical characteristics of the Cambrian-Lower Ordovician and Middle-Upper Ordovician source rocks.The results indicate that the Cambrian gas in the Tazhong uplift is typical cracking gas of sapropelic kerogen.Gas in the Xiaoerbulake Formation is typical over-mature dry gas with a drying coefficient of higher than 0.98 and N₂ content of 2.5%~4.0%.The carbon isotopes of group composition and individual n-alkanes of condensate in the Xiaoerbulake Formation are relatively heavy.The carbon isotope of C₉-C₂₀ n-alkane are -28.8‰~-26.3‰.These geochemistry characteristics indicate that the condensate oil and gas in the Xiaoerbulake Formation originated from the Cambrian-Lower Ordovician source rocks.While the natural gas in the Awatage and Wusonggeer Formations is low-mature wet gas with a drying coefficient of 0.63~0.78 and N₂ content of 0.2%~0.8%.The carbon isotope of group composition and individual n-alkanes of condensate in the Awatage and Wusonggeer Formations are relatively light.The carbon isotopes of C₉-C₂₃ n-alkane are -37.25‰~-32.56‰.These geochemistry characteristics indicate that the condensate oil and gas in the Awatage and Wusonggeer Formations originated from the Middle-Upper Ordovician source rocks.

Key words: gas type, source of oil and gas, organic geochemistry, Cambrian, Tazhong Uplift, Tarim Basin

中图分类号:

TE122.1

史江龙,李剑,李志生,等. 塔里木盆地塔中隆起寒武系深层油气地球化学特征及成因[J]. 石油与天然气地质, 2017, 38(2): 302-310. doi: 10.11743/ogg20170210 Shi Jianglong,Li Jian,Li Zhisheng,et al. Geochemical characteristics and origin of the deep Cambrian oil and gas in the Tazhong Uplift,Tarim Basin[J]. Oil & Gas Geology, 2017, 38(2): 302-310. doi: 10.11743/ogg20170210

参考文献

[1] 漆立新.塔里木盆地下古生界碳酸盐岩大油气田勘探实践与展望[J].石油与天然气地质,2014,35(6):771-779. Qi Lixin.Exploration practice and prospects of giant carbonate field in the Lower Paleozoic of Tarim Basin[J].Oil & Gas Geology,2014,35(6):771-779.
[2] 翟光明,何文渊.塔里木盆地石油勘探实现突破的重要方向[J].石油学报,2004,25(1):1-7. Zhai Guangming,He Wenyuan.An important petroleum exploration region in Tarim Basin[J].Acta Petrolei Sinica,2004,25(1):1-7.
[3] 王招明,谢会文,陈永权,等.塔里木盆地中深1井寒武系盐下白云岩原生油气藏的发现与勘探意义[J].中国石油勘探,2014,19(2):1-13. Wang Zhaoming,Xie Huiwen,Chen Yongquan,et al.Discovery and exploration of Cambrian subsalt dolomite original hydrocarbon reservoir at Zhongshen-1 Well in Tarim Basin[J].China Petroleum Exploration,2014,19(2):1-13.
[4] 顾忆,赵永强,贾存善,等.塔里木盆地阿瓦提坳陷油气资源潜力分析[J].石油实验地质,2012,34(3):257-266. Gu Yi,Zhao Yongqiang,Jia Cunshan,et al.Analysis of hydrocarbon resource potential in Awati Depression of Tarim basin[J].Petroleum Geology & Experiment,2012,34(3):257-266.
[5] 赵靖舟,王清华,时宝宏,等.塔里木古生界克拉通盆地海相油气富集规律与古隆起控油气论[J].石油与天然气地质,2007,28(6):703-712. Zhao Jingzhou,Wang Qinghua,Shi Baohong,et al.Marine hydrocarbon enrichment rules and palaeouplift-controlling hydrocarbon theory for the Paleozoic Tarim craton basin[J].Oil & Gas Geology,2007,28(6):703-712.
[6] 庞雄奇,周新源,李卓,等.塔里木盆地塔中古隆起控油气模式与有利区预测[J].石油学报,2011,32(2):189-198. Pang Xiongqi,Zhou Xinyuan,Li Zhuo,et al.A model for controlling hydrocarbon and predicting favorable exploration zones of the Tazhong palaeo-uplift in Tarim Basin,NW China[J].Acta Petrolei Sinica,2011,32(2):189-198.
[7] 韩剑发,梅廉夫,杨海军,等.塔中Ⅰ号坡折带礁滩复合体大型凝析气田成藏机制[J].新疆石油地质,2008,29(3):323-326. Han Jianfa,Mei Lianfu,Yang Haijun,et al.Hydrocarbon accumulation mechanism of large-sized reef-shoal complex condensate gas field in Tazhong No.1 Slope-Break zone,Tarim Basin[J].Xin Jiang Petroleum Geology,2008,29(3):323-326.
[8] 宋到福,王铁冠,李美俊.塔中地区中深1和中深1C井盐下寒武系油气地球化学特征及其油气源判识[J].中国科学:地球科学,2016,46(1):107-117. Song Daofu,Wang Tieguan,Li Meijun.Geochemistry and possible origin of the hydrocarbons from Wells Zhongshen1 and Zhongshen1C,Tazhong Uplift[J].Science in China:Earth Sciences,2016,46(1):107-117.
[9] 戴金星.中国含硫化氢的天然气分布特征、分类及其成因探讨[J].沉积学报,1985,3(4):109-120. Dai Jinxing.Distribution,classification and origin of natural gas with hydrogen sulphide in China[J].Acta Sedimentologica Sinica,1985,3(4):109-120.
[10] Littke R,Krooss B,Idiz E,et al.Molecular nitrogen in natural gas accumulations:generation from sedimentary organic matter at high temperatures[J].AAPG Bulletin,1995,79(3):410-430.
[11] 刘全有,戴金星,刘文汇,等.塔里木盆地天然气中氮地球化学特征与成因[J].石油与天然气地质,2007,28(1):13-16. Liu Quanyou,Dai Jinxing,Liu Wenhui,et al.Geochemical characteristics and genesis of nitrogen in natural gas from Tarim Basin[J].Oil & Gas Geology,2007,28(1):13-16.
[12] 赵孟军.塔里木盆地和田河气田天然气的特殊来源及非烃组分的成因[J].地质论评,2002,48(5):480-486. Zhao Mengjun.Special source of the natural gases of the Hotan river gas field and the origin of its non-hydrocarbon gases[J].Geological Review,2002,48(5):480-486.
[13] 李谨,李志生,王东良.塔里木盆地含氮天然气地球化学特征及氮气来源[J].石油学报,2013,34(增刊1):102-111. Li Jin,Li Zhisheng,Wang Dongliang.Geochemical characteristics and N₂ source of nitrogen riched natural gas in Tarim Basin[J].Acta Petrolei Sinica,2013,34(S 1):102- 111.
[14] 王鹏,沈忠明,刘四兵,等.四川盆地陆相天然气地球化学特征及对比[J].天然气地球科学,2013,24(6):1186-1195. Wang Peng,Shen Zhongmin,Liu Sibing,et al.The geochemical characteristics and comparison of the terrestrial natural gas in Sichuan Basin[J].Natural Gas Geoscience,2013,24(6):1186-1195.
[15] 张敏,黄光辉,胡国艺,等.原油裂解气和干酪根裂解气的地球化学研究(Ⅰ)-模拟实验和产物分析[J].中国科学D辑:地球科学,2008,38(增刊Ⅱ):1-8. Zhang Min,Huang Guanghui,Hu Guoyi,et al.Study on the geoche-mical characteristics of oil-cracking gas and kergen-cracking gas(Ⅰ):Simulation and product analysis[J].Science in China:Series D,2008,38(S Ⅱ):1-8.
[16] 戴金星.各类烷烃气的鉴别[J].中国科学:B辑,1992,(2):185-193. Dai Jinxing.Discrimination of all kinds of alkane gas[J].Science in China:Series B,1992,(2):185-193.
[17] 戴金星.天然气碳氢同位素特征和各类天然气鉴别[J].天然气地球科学,1993,4(2):1-40. Dai Jinxing.The characteristics of natural gas hydrocarbon isotopic and identification of all kinds of natural gas[J].Natural Gas Geo-science,1993,4(2):1-40.
[18] 戴金星,于聪,黄士鹏,等.中国大气田的地质和地球化学若干特征[J].石油勘探与开发,2014,41(1):1-13. Dai Jinxing,Yu Cong,Huang Shipeng,et al.Geological and geoche-mical characteristics of large gas fields in China[J].Petroleum Exploration and Development,2014,41(1):1-13.
[19] 张殿伟,刘文汇,郑建京,等.塔中地区天然气氦、氩同位素地球化学特征[J].石油勘探与开发,2005,32(6):38-41. Zhang Dianwei,Liu Wenhui,Zheng Jianjing,et al.Helium and argon isotopic compositions of natural gases in the Tazhong area,Tarim Basin[J].Petroleum Exploration and Development,2005,32(6):38-41.
[20] 王铁冠,宋到福,李美俊,等.塔里木盆地海顺南-古城地区奥陶系鹰山组天然气气源与深层天然气勘探前景[J].石油与天然气地质,2014,35(6):753-762. Wang Tieguan,Song Daofu,Li Meijun,et al.Natural gas source and deep gas exploration potential of the Ordovician Yingshan Formation in the Shunnan-Gucheng region,Tarim Basin[J].Oil and Gas Geology,2014,35(6):753-762.
[21] Sofer Z.Stable carbon isotope composition of crude oils:Application to source depositional environments and petroleum alteration[J].AAPG Bulletin,1984,68(1):31-49.
[22] Chung H M,Roonney M A,Toon M B,et al.Carbon isotope composition of marine crude oils[J].AAPG Bulletin,1992,76(2):1000-1007.
[23] Hill R J,Tang Y C,Kaplan I R.Insights into oil cracking based on laboratory experiments[J].Organic Geochemistry,2003,34:1651-1672.
[24] 黄光辉,张敏,胡国艺,等.原油裂解气和干酪根裂解气的地球化学研究(Ⅱ)-原油裂解气和干酪根裂解气的区分方法[J].中国科学D辑:地球科学,2008,38(增刊Ⅱ):9-16. Huang Guanghui,Zhang Min,Hu Guoyi,et al.Geochemical study on oil-cracked gases (Ⅱ):Discrimination methods between oil-cracked gases and kerogen-cracked gases[J].Science in China:Series D,Earth Sciences,2008,38(SⅡ):9-16.
[25] 王云鹏,赵长毅,王兆云,等.海相不同母质来源天然气的鉴别[J].中国科学D辑:地球科学,2007,37(增刊Ⅱ):125-140. Wang Yunpeng,Zhao Changyi,Wang Zhaoyun,et al.Identification of natural gas from different marine sources[J].Science in China:Series D,Earth Sciences,2007,37(SⅡ):125-140.
[26] 张水昌,高志勇,李建军,等.塔里木盆地寒武系-奥陶系海相烃源岩识别与分布预测[J].石油勘探与开发,2012,39(3):285-294. Zhang Shuichang,Gao Zhiyong,Li Jianjun,et al.Identification and distribution of marine hydrocarbon source rocks in the Ordovician and Cambrian of the Tarim Basin[J].Petroleum Exploration and Deve-lopment,2012,39(3):285-294.
[27] 高志勇,张水昌,张兴阳,等.塔里木盆地寒武系-奥陶系海相烃源岩空间展布与层序类型的关系[J].科学通报,2007,52(增刊Ⅰ):70-77. Gao Zhiyong,Zhang Shuichang,Zhang Xingyang,et al.Relations between spatial distribution and sequence types of the Cambrian-Ordovician marine source rocks in Tarim Basin[J].Chinese Science Bulletin,2007,52(SⅠ):70-77.
[28] 刘全有,金之钧,王毅,等.塔里木盆地天然气成因类型与分布规律[J].石油学报,2009,30(1):46-50. Liu Quanyou,Jin Zhijun,Wang Yi,et al.Genetic type and distribution of natural gas in Tarim Basin[J].Acta Petrolei Sinica,2009,30(1):46-50.
[29] 李剑,谢增业,罗霞,等.塔里木盆地主要天然气藏的气源判识[J].天然气工业,1999,19(2):38-43. Li Jian,Xie Zengye,Luo Xia,et al.Gas-source identification of the major gas reservoirs in Tarim Basin[J].Natural Gas Industry,1999,19(2):38-43.
[30] 云金表,金之钧,解国军.塔里木盆地下古生界主力烃源岩分布[J].石油与天然气地质,2014,35(6):827-838. Yun Jinbiao,Jin Zhijun,Xie Guojun.Distribution of major hydrocarbon source rocks in the Lower Palaeozoic,Tarim Basin[J].Oil & Gas Geology,2014,35(6):827-838.
[31] 赵文智,王兆云,王东良,等.分散液态烃的成藏地位与意义[J].石油勘探与开发,2015,42(4):401-413. Zhao Wenzhi,Wang Zhaoyun,Wang Dongliang,et al.Contribution and significance of dispersed liquid hydrocarbons to reservoir formation[J].Petroleum Exploration and Development,2015,42(4):401-413.
[32] 李剑,王义凤,马卫,等.深层-超深层古老烃源岩滞留烃及其裂解气资源评价[J].天然气工业,2015,35(11):9-15. Li Jian,Wang Yifeng,Ma Wei,et al.Evaluation on occluded hydrocarbon in deep-ultra deep ancient source rocks and its cracked gas resources[J].Natural Gas Industry,2015, 35(11):9-15.
[33] Prinzhofer A A,Mello M R,Takaki T.Geochemical characterization of natural gas:a physical multivariable approach and its applications in maturity and migration estimates.AAPG Bulletin,2000,(84):1152-1172.

塔里木盆地塔中隆起寒武系深层油气地球化学特征及成因

Geochemical characteristics and origin of the deep Cambrian oil and gas in the Tazhong Uplift,Tarim Basin

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