黄骅坳陷大港探区深层天然气成因类型与分布规律

doi:10.7623/syxb2013S1013

石油学报 ›› 2013, Vol. 34 ›› Issue (增刊一): 112-119.DOI: 10.7623/syxb2013S1013

黄骅坳陷大港探区深层天然气成因类型与分布规律

国建英¹, 李剑¹, 于学敏², 王东良¹, 付立新², 郝爱胜¹, 崔会英¹

1. 中国石油勘探开发研究院廊坊分院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;
2. 中国石油大港油田公司勘探开发研究院天津大港 300280

收稿日期:2013-03-26 修回日期:2013-07-01 出版日期:2013-09-25 发布日期:2013-09-15
通讯作者: 国建英
作者简介:国建英,男,1971年12月生,2002年获河北大学学士学位,2009年获中国矿业大学(北京)博士学位,现为中国石油勘探开发研究院廊坊分院高级工程师,主要从事油气地球化学及成藏研究工作。Email:gjy_17711224@petrochina.com.cn
基金资助:
国家重大科技专项(2011ZX05007)资助

Origin and distribution of deep natural gas in Dagang exploration area of Huanghua depression

GUO Jianying¹, LI Jian¹, YU Xuemin², WANG Dongliang¹, FU Lixin², HAO Aisheng¹, CUI Huiying¹

1. Langfang Branch, PetroChina Research Institute of Exploration and Development; CNPC Key Laboratory of Gas Reservoir Formation and Development, Langfang 065007, China;
2. Research Institute of Exploration and Development, PetroChina Dagang Oilfield Company, Dagang 300280, China

Received:2013-03-26 Revised:2013-07-01 Online:2013-09-25 Published:2013-09-15

摘要/Abstract

摘要：

通过综合应用天然气组分、碳同位素、氢同位素、轻烃及岩石热解碳同位素等地球化学参数,结合地质背景分析,对大港探区深层天然气的成因类型、来源及分布规律进行了研究。结果表明,大港探区深层天然气以热成因气为主,主要处于成熟—高成熟阶段;按母质类型及来源可进一步划分为煤成气、非煤成煤型气和油型气。深层天然气的分布严格受源岩的控制,煤成气分布于探区中南部的埕北地区、孔店地区及孔南地区;非煤成煤型气主要分布在中北部地区,包括板桥次凹、歧口主凹中北部及夹于这2个凹陷间的北大港潜山构造带;油型气主要分布在歧口主凹的南部、歧北次凹和歧南次凹及其周缘。煤成气主要来自石炭系—二叠系煤系烃源岩,非煤成煤型气和油型气主要来自古近系沙河街组二、三段烃源岩。大港探区深层天然气勘探前景广阔。

关键词: 深层天然气, 地球化学, 成因类型, 分布规律, 大港探区, 黄骅坳陷

Abstract:

This study investigates origin, distribution, and source of deep natural gas in Dagang Exploration Area (DEA), Huanghua depression through a combined analysis of available geochemical data (natural gas compositions, carbon and hydrogen isotopes, light hydrocarbons, and rock-pyrolytic carbon isotope) and geological setting. Results show that deep natural gas in DEA is dominated by thermogenic gas at the stage of maturity-high maturity, which can be classified into three types in terms of type and source of parent materials, i.e., coal-derived gas, coal-type gas, and oil-type gas. The distribution of deep natural gas is strictly controlled by availability of source rocks. Coal-derived gas is mainly distributed in Chengbei, Kongdian, and Kongnan areas in the middle-southern part of DEA.Coal-type gas is mainly distributed in the middle-northern part of DEA, including Banqiao sub-sag, middle-northern Qikou sag, and the northern Dagang buried hill belt inbetween. Oil-type gas mainly occurs in southern Qikou sag, Qibei sub-sag, and periphery of Qinan sub-sag. Coal-derived gas is mainly generated from Carboniferous-Permian source rocks, while coal-and oil-type gases are mainly generated from the second and third members of the Paleogene Shahejie Formation. This work demonstrates that DEA is of great potential for deep gas exploration.

Key words: deep natural gas, geochemistry, gas origin, distribution pattern, Dagang exploration area, Huanghua depression

中图分类号:

TE112.11

国建英, 李剑, 于学敏, 王东良, 付立新, 郝爱胜, 崔会英. 黄骅坳陷大港探区深层天然气成因类型与分布规律[J]. 石油学报, 2013, 34(增刊一): 112-119.

GUO Jianying, LI Jian, YU Xuemin, WANG Dongliang, FU Lixin, HAO Aisheng, CUI Huiying. Origin and distribution of deep natural gas in Dagang exploration area of Huanghua depression[J]. Editorial office of ACTA PETROLEI SINICA, 2013, 34(增刊一): 112-119.

参考文献

[1] 何海清,王兆云,韩品龙.渤海湾盆地深层油气藏类型及油气分布规律[J].石油勘探与开发,1998,25(3):6-9. He Haiqing,Wang Zhaoyun,Han Pinlong.Deep zone reservoir type and oil-gas distribution pattern in Bohai Gulf Basin[J].Petroleum Exploration and Development,1998,25(3):6-9.
[2] 康竹林.渤海湾盆地深层油气勘探前景[J].石油勘探与开发,1996,23(6):20-22. Kang Zhulin.Exploration potential for deep hydrocarbon zones in Bohai Guif Basin[J].Petroleum Exploration and Development,1996,23(6):20-22.
[3] 胡海燕.深部油气成藏机理概论[J].大庆石油地质与开发,2006,25(6):24-26. Hu Haiyan.Deep hydrocarbon reservoir formation mechanism survey[J].Petroleum Geology & Oilfield Development in Daqing,2006,25(6):24-26.
[4] 杨池银.千米桥潜山凝析气藏天然气成因分析[J].江汉石油学院学报,2004,26(1):35-36. Yang Chiyin.Analysis of natural gas genesis in buried hill condensate gas reservoirs of Qianmiqiao[J].Journal of Jianghan Petroleum Institute,2004,26(1):35-36.
[5] 李剑,胡国艺,谢增业,等.中国大中型气田天然气成藏物理化学模拟研究[M].北京:石油工业出版社,2001:96-100. Li Jian,Hu Guoyi,Xie Zengye,et al.Study of gas accumulation physical and chemistry simulation in China's large and medium gas fields[M].Beijing:Petroleum Industry Press,2001:96-100.
[6] 杨池银.板桥凹陷深层天然气气源对比与成因分析[J].天然气地球科学,2003,14(1):83-88. Yang Chiyin.Nature gas source correlation and its genesis analysis for the deep gas pool in Banqiao sag[J].Natural Gas Geoscience,2003,14(1):83-88.
[7] 姜平.千米桥潜山构造凝析油气藏成因[J].天然气工业,2001,21(4):39-43. Jiang Ping.Condensate reservoir formation in Qianmiqiao buried hill structure[J].Natural Gas Industry,2001,21(4):39-43.
[8] 张亚光,杨子玉,肖枚,等.乌马营潜山天然气藏地质地球化学特征和成藏过程[J].天然气地球科学,2003,14(4):283-286. Zhang Yaguang,Yang Ziyu,Xiao Mei,et al.Wumaying Buried Hill gas reservoir geological and geochemical characters and origin analysis[J].Natural Gas Geoscience,2003,14(4):283-286.
[9] 杨池银.黄骅坳陷二氧化碳成因研究[J].天然气地球科学,2004,15(1):7-11. Yang Chiyin.Study on the genesis of CO₂ in Huanghua depression[J].Natural Gas Geoscience,2004,15(1):7-11.
[10] 金振奎,白武厚,张响响.黄骅坳陷二氧化碳气成因类型及分布规律[J].地质科学,2003,38(3):350-360. Jin Zhenkui,Bai Wuhou,Zhang Xiangxiang.Genetic types and distribution of carbon dioxide in the Huanghua depression[J].Chinese Journal of Geology,2003,38(3):350-360.
[11] 武战国,于志海.黄骅坳陷二氧化碳气成因类型及富集规律[J].中国石油勘探,2007,12(1):43-48. Wu Zhanguo,Yu Zhihai.Genetic type and concentration regularity of carbon dioxide gas in Huanghua depression[J].China Petroleum Exploration,2007,12(1):43-48.
[12] 戴春森,宋岩,杨池银.黄骅坳陷天然气中多成因二氧化碳的判识及其混合模型[J].石油勘探与开发,1994,21(4):23-29.Dai Chunsen,Song Yan,Yang Chiyin.A mixed model for polyoriginal carbon dioxide of natural gas in Huanghua depression[J].Petroleum Exploration and Development,1994,21(4):23-29.
[13] 丁巍伟,戴金星,陈汉林,等.黄骅坳陷新生代构造活动对无机成因CO₂气藏控制作用的研究[J].高校地质学报,2004,10(4):616-623.Ding Weiwei,Dai Jinxing,Chen Hanlin,et al.Cenozoic tectonic control on the abiogenic CO₂ gas deposits,Huanghua depression[J].Geological Journal of China Universities,2004,10(4):616-623.
[14] 国建英,于学敏,李剑,等.歧口凹陷歧深1井气源综合对比[J].天然气地球科学,2009,20(3):392-399.Guo Jianying,Yu Xuemin,Li Jian,et al.Gas source of Qishen1 well in Qikou sag[J].Natural Gas Geoscience,2009,20(3):392-399.
[15] 王振升,于学敏,国建英,等.歧口凹陷天然气地球化学特征及成因分析[J].天然气地球科学,2010,21(4):683-691. Wang Zhensheng,Yu Xuemin,Guo Jianying,et al.Geochemical characteristics and genesis of natural gas in Qikou sag [J].Natural Gas Geoscience,2010,21(4):683-691.
[16] 国建英,钟宁宁,于学敏,等.歧口凹陷烷烃气碳、氢同位素特征及成因类型[J].天然气地球科学,2011,22(6):1054-1063.Guo Jianying,Zhong Ningning,Yu Xuemin,et al.Characteristics of carbon and hydrogen isotopes and genetic type of hydrocarben gases in Qikou sag[J].Natural Gas Geoscience,2011,22(6):1054-1063.
[17] 吴永平,于学敏.黄骅坳陷天然气资源潜力与勘探开发对策[J].天然气地球科学,2003,14(4):235-239. Wu Yongping,Yu Xuemin.Nature gas resourse potential and the strategy of exploration and development in Huanghua depression [J].Natural Gas Geoscience,2003,14(4):235-239.
[18] 宋岩.中国天然气资源分布特征与勘探方向[J].天然气工业,2003,3(1):1-4.Song Yan.Distribution characteristics and exploration trend of natural gas resources in China [J].Natural Gas Industry,2003,3(1):1-4.
[19] 戴金星.各类烷烃气的鉴别[J].中国科学B辑:化学,1992,22(2):185-193. Dai Jinxing.The identification of all kinds of alkane gas[J].Science in China Series B:Chemistry,1992,22(2):185-193.
[20] Thompson K F M.Light hydrocarbons in subsurface sediments[J].Geochimica et Cosmochimica Acta,1979,43(5):657-672.
[21] 蒋助生,胡国艺,李志生,等.鄂尔多斯盆地古生界气源对比新探索[J].沉积学报,1999,17(增刊):820-824. Jiang Zhusheng,Hu Guoyi,Li Zhisheng,et al.The novel approach of the correlation between paleozoic natural gas and source rock in Ordos Basin[J].Acta Sedimentologica Sinica,1999,17(Supplement):820-824.
[22] 胡国艺,李剑,李谨,等.判识天然气成因的轻烃指标探讨[J].中国科学D辑:地球科学,2007,37(增刊):111-117. Hu Guoyi,Li Jian,Li Jin,et al.Preliminary study on the origim identification of natural gas by the parameters of light hydrocarbon[J].Science in China Series D:Earth Sciences,2008,51(Supplement 1):131-139.
[23] 王一刚,窦立荣,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. Wang Yigang,Dou Lirong,Ying Chu,et al.Origin of in Triassic Feixianguan Formation gas pools,northeastern Sichuan Basin,China[J].Geochimica,2002,31(6):517-524.
[24] 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):349-352. Yang Jiajing,Wang Yigang,Wang Lansheng,et al.The origin of natural gases and geochemistry characters of Changxing reef and Feixianguan oolitic beach gas reservoirs in eastern Sichuan Basin[J].Acta Sedimentologica Sinica,2002,20(2):349-352.
[25] 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.
[26] 朱光有,张水昌,梁英波,等.川东北地区飞仙关组高含H2S天然气TSR成因的同位素证据[J].中国科学D辑:地球科学,2005,35(11):1037-1046.Zhu Guangyou,Zhang Shuichang,Liang Yingbo,et al.The isotopic evidence of TSR origination with hydrogen sulfide bearing gas of Feixianguan Formation in northeastern Sichuan Basin[J].Science in China Series D:Earth Science,2005,35(11):1037-1046.
[27] 朱光有,张水昌,李剑,等.中国高含硫化氢天然气的形成及其分布[J].石油勘探与开发,2004,31(4):18-21. Zhu Guangyou,Zhang Shuichang,Li Jian,et al.Formation and distribution of hydrogen sulfide bearing gas in China[J].Petroleum Exploration and Development,2004,31(4):18-21.
[28] 朱光有,戴金星,张水昌,等.含硫化氢天然气的形成机制及分布规律研究[J].天然气地球科学,2004,15(2):166-170.Zhu Guangyou,Dai Jinxing,Zhang Shuichang,et al.Generation mechanism and distribution characteristics of hydrogen sulfide bearing gas in China[J].Natural Gas Geoscience,2004,15(2):166-170.
[29] 于超,苏俊青,钱茂路,等.滨海断鼻古近系油气藏分布特征与控制因素浅析[J].天然气地球科学,2010,21(4):547-553. Yu Chao,Su Junqing,Qian Maolu,et al.Distribution and controlling factors of eogene oil & gas reservoirs in Binhai fault nose zone[J].Natural Gas Geoscience,2010,21(4):547-553.

黄骅坳陷大港探区深层天然气成因类型与分布规律

Origin and distribution of deep natural gas in Dagang exploration area of Huanghua depression

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