天然气地球科学

• 天然气地球化学 • 上一篇    下一篇

川中地区须家河组天然气氢同位素特征及其对水体咸化的指示意义

倪云燕1,2,廖凤蓉1,2,姚立邈1,2,高金亮1,2,张蒂嘉1,2   

  1. 1.中国石油天然气股份有限公司油气地球化学重点实验室,北京 100083;
    2.中国石油勘探开发研究院,北京 100083
  • 收稿日期:2019-04-29 修回日期:2019-05-29 出版日期:2019-06-10
  • 作者简介:倪云燕(1977-),女,浙江乐清人,高级工程师,博士,主要从事油气地球化学研究.E-mail:niyy@petrochina.com.cn.
  • 基金资助:
    国家自然科学基金(编号:41472120);国家科技重大专项课题(编号:2016ZX05-007)联合资助。

Stable hydrogen isotopic characteristics of natural gas from the Xujiahe Formation in the central Sichuan Basin and its implications for water salinization 

Ni Yun-yan1,2,Liao Feng-rong1,2,Yao Li-miao1,2,Gao Jin-liang1,2,Zhang Di-jia1,2   

  1. 1. Key Laboratory of Petroleum Geochemistry,China National Petroleum Corporation,Beijing 100083,China;
    2. PetroChina Research Institute of Petroleum Exploration & Development,Beijing 100083,China
  • Received:2019-04-29 Revised:2019-05-29 Online:2019-06-10

摘要: 通过对四川盆地川中地区须家河组天然气的组分和碳氢同位素分析,结合前人对川西和川南地区须家河组及四川盆地其他层系天然气研究成果和区域地质背景,开展天然气成因和来源、氢同位素特征与指示意义等研究。结果表明,川中地区须家河组天然气以烃类气体为主,甲烷含量为67.89%~98.05%,重烃气(C2+)含量为0.42%~16.62%,非烃气体(CO2、N2)含量较低,除岳121井N2和CO2含量较高外,N2含量平均值为0.82%,CO2含量平均值为0.26%。元坝须家河组天然气干燥系数平均高达0.991,为干气;川中其他地区须家河组天然气干燥系数皆小于0.95,为湿气。天然气δ13C1值介于-43.8‰~-29.2‰之间,δ13C2值介于-33.5‰~-20.7‰之间,δ13C3值介于-33.6‰~-19.3‰之间,δ13C4值介于为-27.2‰~-22.2‰之间;天然气δD1值介于-191‰~-148‰之间,δD2值介于-165‰~-115‰之间,δD3值介于-153‰~-107‰之间。甲烷及其同系物(C2-4)基本上为碳氢同位素正序排列(δ13C113C213C313C4、δD1<δD2<δD3),与典型的有机成因烷烃气碳氢同位素特征一致。元坝须家河组天然气成熟度RO值为1.09%~1.78%,川中其他地区须家河组天然气成熟度RO值为0.64%~0.92%。川中须家河组天然气主要为来自须家河组煤系源岩的煤成气,元坝须二段天然气为来自须家河组煤系源岩的高成熟煤成气混入下寒武统(及下志留统)原油裂解气的混合气。四川盆地须家河组天然气甲烷δD值偏高,都大于-200‰。与来自淡水湖沼相烃源岩的吐哈盆地台北凹陷的煤成气相比,尽管两者成熟度相近,但甲烷δD值差异高达90‰,说明须家河组煤系源岩形成于水体咸化的沉积环境。

关键词: 四川盆地, 川中地区, 须家河组, 碳同位素, 氢同位素, 水体咸化

Abstract: Based on the analysis of the components and carbon and hydrogen isotopes of gases from the Triassic Xujiahe and other formations in the Sichuan Basin,the gas origin,gas source and significance of hydrogen isotopes are studied by combining previous research results and regional geological background. The results show that gas from the Triassic Xujiahe Formation in the Sichuan Basin is mainly hydrocarbon gas. The content of methane is 67.89%-98.05%,and the content of heavy hydrocarbon (C2+) is 0.42%-16.62%. The content of non-hydrocarbon gas (CO2,N2) is low. Except the relatively high content of N2 and CO2 in the Well Yue121,the average content of N2 is 0.82% and the average value of CO2 is 0.26%. Gas from the Xujiahe Formation in Yuanba has average dryness coefficient as high as 0.991,which indicates the gas belongs to dry gas. While,gases from the Xujiahe Formation in other areas in the Central Sichuan Basin have dryness coefficient less than 0.95,indicative of wet gas. The δ13C1 value varies from -43.8‰ to -29.2‰,δ13C2 value ranges from -33.5‰ to -20.7‰,δ13C3 value is from -33.6‰ to -19.3‰ and δ13C4 value is from -27.2‰ to -22.2‰. The δD1 value is from -191‰ to -148‰,δD 2value is from -165‰ to -115‰ and δD3 value is from -153‰ to -107‰. Methane and its homologues (C2-4) become more enriched in 13C and D with increasing carbon number (δ13C113C213C313C4,δD1<δD2<δD3),which are consistent with the carbon and hydrogen isotopic characteristics of thermogenic gases. The thermal maturity Rof natural gas from Xujiahe Formation in Yuanba is 1.09%-1.78%,and the RO of the natural gas from Xujiahe Formation in other areas of Central Sichuan Basin is 0.64%-0.92%. Natural gas from the Xujiahe Formation in the central Sichuan Basin is mainly from the coal measure source rocks of the Xujiahe Formation. Natural gas from the 2nd member of Xujiahe Formation in Yuanba is mixed gas,a mixture of the high-mature coal-derived gas from the coal measure source rock of Xujiahe Formation and the Lower Cambrian (Lower Silurian) oil-cracked gas. The δD of methane from the Xujiahe Formation in the Sichuan Basin is relatively high,higher than -200‰. Compared to the coal-derived gas from the source rocks formed in limnetic facies with freshwater in the Taibei Sag,Turpan-Hami Basin,though at similar thermal maturity,the difference of the δD of methane can be as high as 90‰,indicating that the source rock of Xujiahe Formation is formed in an environment with water salinization.

Key words: Sichuan Basin, Central Sichuan Basin, Xujiahe Formation, Carbon isotope, Hydrogen isotope, Water salinization

中图分类号: 

  • T122.1+13
[1]Dai Jinxing.Coal-derived gas theory and its discrimination[J].Chinese Science Bulletin,2018,63(14):1291-1305.
戴金星.煤成气及鉴别理论研究进展[J].科学通报,2018,63(14):1291-1305.
[2]Ni Yunyan,Ma Qisheng,Ellis G S,et al.Fundamental studies on kinetic isotope effect (KIE) of Hydrogen isotope fractionation in natural gas systems[J].Geochimica et Cosmochimica Acta,2011,75(10):2696-2707.
[3]Ni Yunyan,Zhang Dijia,Liao Fengrong,et al.Stable hydrogen and carbon isotopic ratios of coal-derived gases from the Turpan-Hami Basin,NW China[J].International Journal of Coal Geology,2015,152:144-155.
[4]Dai Jinxing.Characteristics of carbon and hydrogen isotopes of natural gases and their discriminations[J].Natural Gas Geoscience,1993,4(2/3):1-40.
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(2/3):1-40.
[5]Wang Wanchun.Geochemical characteristics of hydrogen isotopic compositions of natural gas,oil and kerogen[J].Acta Sedimentologic Sinica,1996,14(S1):131-135.
王万春.天然气、原油、干酪根的氢同位素地球化学特征[J].沉积学报,1996,14(S1):131-135.
[6]Liu Quanyou,Dai Jinxing,Li Jian,et al.Hydrogen isotope composition of natural gases from the Tarim Basin and its indication of depositional environments of the source rocks[J].Science in China:Series D,2007,37(12):1599-1608.
刘全有,戴金星,李剑,等.塔里木盆地天然气氢同位素地球化学与对热成熟度和沉积环境的指示意义[J].中国科学:D辑,2007,37(12):1599-1608.
[7]Schoell M.The Hydrogen and Carbon isotopic composition of methane from natural gases of various origins[J].Geochimica et Cosmochimica Acta,1980,44(5):649-661.
[8]Dai Jinxing,Ni Yunyan,Zou Caineng.Stable carbon and hydrogen isotopes of natural gases sourced from the Xujiahe Formation in the Sichuan Basin,China[J].Organic Geochemistry,2012,43:103-111.
[9]Shen Ping,Xu Yongchang.The isotopic composition of natural gases from continental sediments in China[J].Geochimica,1991,20(2):144-152.
沈平,徐永昌.中国陆相成因天然气同位素组成特征[J].地球化学,1991,20(2):144-152.
[10]Wang Xiaofeng,Liu Wenhui,Shi Baoguang,et al.Hydrogen isotope characteristics of thermogenic methane in Chinese sedimentary basins[J].Organic Geochemistry,2015,(83/84):178-189.
[11]Ni Yunyan,Liao Fengrong,Gao Jinliang,et al.Hydrogen isotopes of hydrocarbon gases from different organic facies of the Zhongba Gas Field,Sichuan Basin,China[J].Journal of Petroleum Science and Engineering,2019,179:776-786.
[12]Wang Xiaofeng,Liu Wenhui,Xu Yongchang,et al.Influences of water media on the hydrogen isotopic composition of natural gas/methane in the processes of gaseous hydrocarbon generation and evolution[J].Science in China:Series D,2011,54(9):1318-1325.
王晓锋,刘文汇,徐永昌,等.水介质对气态烃形成演化过程氢同位素组成的影响[J].中国科学:D辑,2012,42(1):103-110.
[13]Li Xizhe,Zhang Manlang,Xie Wuren,et al.Sedimentary facies of Upper Triassic Xujiahe Formation in southwest Sichuan Basin[J].Natural Gas Industry,2008,28(2):54-57,165.李熙喆,张满郎,谢武仁,等.川西南地区上三叠统须家河组沉积相特征[J].天然气工业,2008,28(2):54-57,165.
[14]Zhang Jinliang,Wang Baoqing.Sedimentary facies of Upper Triassic in western Sichuan Basin[J].Journal of Xi'an Petroleum Institute:Natural Science Edition,2000,15(2):1-6,60.
张金亮,王宝清.四川盆地中西部上三叠统沉积相[J].西安石油学院学报:自然科学版,2000,15(2):1-6,60.
[15]Shi Zhensheng,Yang Wei,Jin Hui,et al.Study on sedimentary facies of the Upper Triassic in central and south Sichuan Province[J].Acta Sedimentologica Sinica,2008,26(2):211-220.
施振生,杨威,金惠,等.川中—川南地区上三叠统沉积相研究[J].沉积学报,2008,26(2):211-220.
[16]Shi Zhensheng,Xie Wuren,Ma Shiyu,et al.Transgression sedimentary records of the members 4-6 of Upper Triassic Xujiahe Formation in Sichuan Basin[J].Journal of Palaeogeography,2012,14(5):583-595.
施振生,谢武仁,马石玉,等.四川盆地上三叠统须家河组四段—六段海侵沉积记录[J].古地理学报,2012,14(5):583-595.
[17]Zhao Xiafei,Lv Zonggang,Zhang Wenlin,et al.Paralic tidal deposits in the Upper Triassic Xujiahe Formation in Anyue area,the Sichuan Basin[J].Natural Gas Industry,2008,28(4):14-18,134.
赵霞飞,吕宗刚,张闻林,等.四川盆地安岳地区须家河组——近海潮汐沉积[J].天然气工业,2008,28(4):14-18,134.
[18]Zhang Min,Huang Guanghui,Li Hongbo,et al.Molecular geochemical characteristics of gas source rocks from the Upper Triassic Xujiahe Formation indicate transgression events in the Sichuan Basin[J].Science in China:Series D,2012,55(8):1260-1268.
[19]Zhai Guangming.Petroleum Geology of China (Volume 10)-Sichuan Oil & Gas Fields[M].Beijing:Petroleum Industry Press,1990:516.
翟光明.中国石油地质志(卷十)---四川油气区[M].北京:石油工业出版社,1990:516.
[20]Qin Qirong,Su Peidong,Li Le,et al.Origin of low structures in central Sichuan area[J].Xinjiang Petroleum Geology,2005,26(1):108-111.
秦启荣,苏培东,李乐,等.川中低缓构造成因[J].新疆石油地质,2005,26(1):108-111.
[21]Chen Yicai,Guo Gui’an,Jiang Yujiang,et al.Geochemical features of natural gas and the process of Upper Triassic hydrocarbon accumulation in middle Sichuan area[J].Natural Gas Geoscience,2007,18(5):737-742.
陈义才,郭贵安,蒋裕强,等.川中地区上三叠统天然气地球化学特征及成藏过程探讨[J].天然气地球科学,2007,18(5):737-742.
[22]Xiao Zhihua,Xie Zengye,Li Zhisheng,et al.Isotopic characteristics of natural gas of Xujiahe Formation in southern and middle of Sichuan Basin[J].Geochimica,2008,37(3):245-250.
肖芝华,谢增业,李志生,等.川中—川南地区须家河组天然气同位素组成特征[J].地球化学,2008,37(3):245-250.
[23]Wang Lansheng,Chen Chengji,Du Min,et al.Organic geochemistry chacteristics and resources potential of Triassic natural gas in Sichuan Basin,China[J].Natural Gas Geoscience,2008,19(2):222-228.
王兰生,陈盛吉,杜敏,等.四川盆地三叠系天然气地球化学特征及资源潜力分析[J].天然气地球科学,2008,19(2):222-228.
[24]Tang Yue,Wang Liangliang,Cui Zehong.An analysis of the gas source in the Upper Triassic Xujiahe Formation,central Sichuan Basin[J].Geological Bulletin of China,2011,30(10):1608-1613.
唐跃,王靓靓,崔泽宏.川中地区上三叠统须家河组气源分析[J].地质通报,2011,30(10):1608-1613.
[25]Yi Shiwei,Lin Shiguo,Yang Wei,et al.Condition of Xujiahe Formation large gas province formation in Sichuan Basin[J].Natural Gas Geoscience,2013,24(1):1-8.
易士威,林世国,杨威,等.四川盆地须家河组大气区形成条件[J].天然气地球科学,2013,24(1):1-8.
[26]Wu Xiaoqi,Huang Shipeng,Liao Fengrong,et al.Carbon isotopic compositions of coal-derived gas in the Xujiahe Formation and Jurassic in the Sichuan Basin[J].Petroleum Exploration and Development,2011,38(4):418-427.
吴小奇,黄士鹏,廖凤蓉,等.四川盆地须家河组及侏罗系煤成气碳同位素组成[J].石油勘探与开发,2011,38(4):418-427.
[27]Wang Shiqian,Luo Qihou,Deng Hongbin,et al.Characteristics of forming Jurassic gas reservoirs in the west part of Sichuan Basin[J].Natural Gas Industry,2001,21(2):1-8,10.王世谦,罗启后,邓鸿斌,等.四川盆地西部侏罗系天然气成藏特征[J].天然气工业,2001,21(2):1-8,10.
[28]Fan Ranxue,Zhou Hongzhong,Cai Kaiping.Carbon isotopic geochemistry and origin of natural gases in the southern part of the western Sichuan Depression[J].Acta Geoscientica Sinic,2005,26(2):157-162.
樊然学,周洪忠,蔡开平.川西坳陷南段天然气来源与碳同位素地球化学研究[J].地球学报,2005,26(2):157-162.
[29]Qin Shengfei,Tao Shizhen,Tu Tao,et al.Characteristics of natural gas geochemistry and accumulation in western Sichuan Depression[J].Petroleum Exploration and Development,2007,34(1):34-38,54.
秦胜飞,陶士振,涂涛,等.川西坳陷天然气地球化学及成藏特征[J].石油勘探与开发,2007,34(1):34-38,54.
[30]Dai Jinxing,Xia Xinyu,Li Zhisheng,et al.Inter-laboratory calibration of natural gas round robins for δ2H and δ13C using off-line and on-line techniques[J].Chemical Geology,2012,(310/311):49-55.
[31]Dai Jinxing.The Giant Coal-Derived Gas Fields and Their Gas Sources in China[M].Beijing:Science Press,2014:424.
戴金星.中国煤成大气田及气源[M].北京:科学出版社,2014:424.
[32]Hu Wei,Zhu Yangming,Li Ying,et al.Geochemical characteristics and origin of natural gases from terrestrial strata in Yuanba area of the northeastern Sichuan Basin[J].Journal of Zhejiang University:Science Edition,2014,41(4):468-476.
胡炜,朱扬明,李颖,等.川东北元坝地区陆相气地球化学特征及来源[J].浙江大学学报:理学版,2014,41(4):468-476.
[33]Wu Xiaoji,Liu Guangxiang,Liu Quanyou,et al.Geochemical characteristics and origin of natural gas in the Xujiahe Formation in Yuanba-Tongnanba area of Sichuan Basin[J].Oil & Gas Geology,2015,36(6):955-962,974.
吴小奇,刘光祥,刘全有,等.四川盆地元坝—通南巴地区须家河组天然气地球化学特征和成因[J].石油与天然气地质,2015,36(6):955-962,974.
[34]Liu Wenhui,Xu Yongchang.A two-stage model of carbon isotopic fractionation in coal-gas[J].Geochimica,1999,28(4):359-366.
刘文汇,徐永昌.煤型气碳同位素演化二阶段分馏模式及机理[J].地球化学,1999,28(4):359-366.
[35]Tao Cheng,Ba Liqiang,Wang Jie,et al.Analysis and application of hydrogen isotopic composition of the natural gas[J].Petroleum Geology & Experiment,2008,30(1):94-97.
陶成,把立强,王杰,等.天然气氢同位素分析及应用[J].石油实验地质,2008,30(1):94-97.
[36]Qian Zhihao,Cao Yin,Zhang Meizhen.Feature of hydrocarbon isotope composition of individual hydrocarbon in natural methane gas from northeast part of Sichuan[J].Marine Origin Petroleum Geology,2008,13(2):17-21.
钱志浩,曹寅,张美珍.川东北天然气单体烃氢同位素组成特征[J].海相油气地质,2008,13(2):17-21.
[37]Dai Jinxing,Xia Xinyu,Qin Shengfei,et al.Origins of partially reversed alkane δ13C values for biogenic gases in China[J].Organic Geochemistry,2004,35(4):405-411.
[38]Marais D D,Donchin J H,Nehring N L,et al.Molecular carbon isotopic evidence for the origin of geothermal hydrocarbons[J].Nature,1981,292(5826):826-828.
[39]Bernard B B,Brooks J M,Sackett W M.Natural gas seepage in the Gulf of Mexico[J].Earth and Planetary Science Letters,1976,31(1):48-54.
[40]Whiticar M J.Carbon and hydrogen isotope systematics of bacterial formation and oxidation of methane[J].Chemical Geology,1999,161(1):291-314.
[41]Dai Jinxing,Pei Xigu,Qi Houfa.Natural Gas Geology in China[M].Beijing:Petroleum Industry Press,1992.
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.
[42]Dai Jinxing,Qin Shengfei,Tao Shizhen,et al.Developing trends of natural gas industry and the significant progress on natural gas geological theories in China[J].Natural Gas Geoscience,2005,16(2):127-142.
戴金星,秦胜飞,陶士振,等.中国天然气工业发展趋势和天然气地学理论重要进展[J].天然气地球科学,2005,16(2):127-142.
[43]Gang Wenzhe,Gao Gang,Hao Shisheng,et al.Carbon isotope of ethane applied in the analyses of genetic types of natural gas[J]. Petroleum Geology & Experiment,1997,19(2):164-167.
刚文哲,高岗,郝石生,等.论乙烷碳同位素在天然气成因类型研究中的应用[J].石油实验地质,1997,19(2):164-167.
[44]Chen Jianfa,Li Chunyuan,Shen Ping,et al.Carbon and hydrogen isotopic characteristics of hydrocarbons in coal type gas from China[J].Acta Sedimentologic Sinica,1995,13(2):59-69.
陈践发,李春园,沈平,等.煤型气烃类组分的稳定碳、氢同位素组成研究[J].沉积学报,1995,13(2):59-69.
[45]Dai Jinxing,Ni Yunyan,Zou Caineng,et al.Stable carbon isotopes of alkane gases from the Xujiahe coal measures and implication for gas-source correlation in the Sichuan Basin,SW China[J].Organic Geochemistry,2009,40(5):638-646.
[46]Dai Jinxing,Ni Yunyan,Wu Xiaoqi.Tight gas in China and its significance in exploration and exploitation[J].Petroleum Exploration and Development,2012,39(3):277-284.
[47]Tang Y,Perry J K,Jenden P D,et al.Mathematical modeling of stable Carbon isotope ratios in natural gases[J].Geochimica et Cosmochimica Acta,2000,64(15):2 268-2673.
[48]Jenden P D,Newell K D,Kaplan I R,et al.Composition and stable-isotope geochemistry of natural gases from Kansas,Midcontinent,U.S.A[J].Chemical Geology,1988,71(1-3):117-147.
[49]Tissot B P,Welte D H.Petroleum Formation and Occurrence[M].2nd ed.Berlin Heidelberg New York Tokyo:Springer-Verlag,1984:699.
[50]Ma Yongsheng.Geochemical characteristics and origin of natural gas from Puguang Gas Field on eastern Sichuan Basin[J].Natural Gas Geoscience,2008,19(1):1-7.
马永生.普光气田天然气地球化学特征及气源探讨[J].天然气地球科学,2008,19(1):1-7.
[51]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.
[52]Dai Jinxing,Liao Fengrong,Ni Yunyan.Discussions on the gas source of the Triassic Xujiahe Formation tight sandstone gas reservoirs in Yuanba and Tongnanba,Sichuan Basin:An answer to Yinfeng et al[J].Petroleum Exploration and Development,2013,40(2):250-256.戴金星,廖凤蓉,倪云燕.四川盆地元坝和通南巴地区须家河组致密砂岩气藏气源探讨——兼答印峰等[J].石油勘探与开发,2013,40(2):250-256.
[53]Dai Jinxing,Qi Houfa.Relationship of δ13C-RO of coal-derived gas in China[J].Chinese Science Bulletin,1989,34(9):690-692.
戴金星,戚厚发.我国煤成烃气的δ13C-RO关系[J].科学通报,1989,34(9):690-692.
[54]Rooney M A,Claypool G E,Chung H M.Modeling thermogenic gas generation using carbon isotope ratios of natural gas hydrocarbons[J].Chemical Geology,1995,126(3/4):219-232.
[55]Yin Feng,Liu Rebing,Qin Hua.About origin of tight sandstone gas:To discuss with academician Dai Jinxing[J].Petroleum Exploration and Development,2013,40(1):125-128.
印峰,刘若冰,秦华.也谈致密砂岩气藏的气源——与戴金星院士商榷[J].石油勘探与开发,2013,40(1):125-128.
[56]Liang Digang,Guo Tonglou,Chen Jianping,et al.Some progresses on studies of hydrocarbon generation and accumulation in marine sedimentary regions,southern China (Part 2):Geochemical characteristics of four suits of regional marine source rocks,south China[J].Marine Origin Petroleum Geology,2009,14(1):1-15.
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.
[57]Chen Jianping,Li Wei,Ni Yunyan,et al.The Permian source rocks in the Sichuan Basin and its natural gas exploration potential (part 2):Geochemical characteristics of source rocks and latent capacity of natural gas resources[J].Natural Gas Industry,2018,38(6):33-45.
陈建平,李伟,倪云燕,等.四川盆地二叠系烃源岩及其天然气勘探潜力(二)——烃源岩地球化学特征与天然气资源潜力[J].天然气工业,2018,38(6):33-45.
[58]Dai Jinxing,Ni Yunyan,Qin Shengfei,et al.Geochemical characteristics of ultra-deep natural gas in the Sichuan Basin,SW China[J].Petroleum Exploration and Development,2018,45(4):588-597.
戴金星,倪云燕,秦胜飞,等.四川盆地超深层天然气地球化学特征[J].石油勘探与开发,2018,45(4):588-597.
[59]Dai Jinxing,Ni Yunyan,Huang Shipeng.Discussion on the carbon isotopic reversal of alkane gases from the Huanglong Formation in the Sichuan Basin,China[J].Acta Petrolei Sinica,2010,31(5):710-717.
戴金星,倪云燕,黄士鹏.四川盆地黄龙组烷烃气碳同位素倒转成因的探讨[J].石油学报,2010,31(5):710-717.
[60]Liang Digang,Guo Tonglou,Chen Jianping,et al.Some progresses on studies of hydrocarbon generation and accumulation in marine sedimentary regions,southern China (Part 1):Distribution of four suits of regional marine source rocks[J].Marine Origin Petroleum Geology,2008,13(2):1-16.
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(一)—南方四套区域性海相烃源岩的分布[J].海相油气地质,2008,13(2):1-16.
[61]Wang Lansheng,Zou Chunyan,Zheng Ping,et al.Geochemical evidence of shale gas existed in the Lower Paleozoic Sichuan Basin[J].Natural Gas Industry,2009,29(5):59-62,138.
王兰生,邹春艳,郑平,等.四川盆地下古生界存在页岩气的地球化学依据[J].天然气工业,2009,29(5):59-62,138.
[62]Huang Wenming,Liu Shugen,Wang Guozhi,et al.Geological conditions and gas reservoir features in Lower Paleozoic in Sichuan Basin[J].Natural Gas Geoscience,2011,22(3):465-476.
黄文明,刘树根,王国芝,等.四川盆地下古生界油气地质条件及气藏特征[J].天然气地球科学,2011,22(3):465-476.
[63]Zou Caineng,Du Jinhu,Xu Chunchun,et al.Formation,distribution,resource potential and discovery of the Sinian-Cambrian giant gas field,Sichuan Basin,SW China[J].Petroleum Exploration and Development,2014,41(3):278-293.
邹才能,杜金虎,徐春春,等.四川盆地震旦系—寒武系特大型气田形成分布、资源潜力及勘探发现[J].石油勘探与开发,2014,41(3):278-293.
[64]Wei Guoqi,Yang Wei,Xie Wuren,et al.Formation conditions,accumulation models and exploration direction of large gas fields in Sinian-Cambrian,Sichuan Basin[J].Natural Gas Geoscience,2015,26(5):785-795.
魏国齐,杨威,谢武仁,等.四川盆地震旦系—寒武系大气田形成条件、成藏模式与勘探方向[J].天然气地球科学,2015,26(5):785-795.
[65]Wei Guoqi,Wang Zhihong,Li Jian,et al.Characteristics of source rocks,resource potential and exploration direction of Sinian and Cambrian in Sichuan Basin[J].Natural Gas Geoscience,2017,28(1):1-13.
魏国齐,王志宏,李剑,等.四川盆地震旦系、寒武系烃源岩特征、资源潜力与勘探方向[J].天然气地球科学,2017,28(1):1-13.
[66]Liu Shugen,Deng Bin,Zhong Yong,et al.Unique geological features of burial and superimposition of the Lower Paleozoic shale gas across the Sichuan Basin and its periphery[J].Earth Science Frontiers,2016,23(1):11-28.
刘树根,邓宾,钟勇,等.四川盆地及周缘下古生界页岩气深埋藏—强改造独特地质作用[J].地学前缘,2016,23(1):11-28.
[67]Xie Zengye,Zhang Benjian,Yang Chunlong,et al.Geochemical characteristics and source trace of the Devonian natural gas and bitumen in northwest Sichuan Basin[J].Acta Petrolei Sinica,2018,39(10):1103-1118.
谢增业,张本健,杨春龙,等.川西北地区泥盆系天然气沥青地球化学特征及来源示踪[J].石油学报,2018,39(10):1103-1118.
[68]Huang Difan,Wang Lansheng.Geochemical characteristics of bituminous dike in Kuangshanliang area of the northwestern Sichuan Basin and its significance[J].Acta Petrolei Sinica,2008,29(1):23-28.
黄第藩,王兰生.川西北矿山梁地区沥青脉地球化学特征及其意义[J].石油学报,2008,29(1):23-28.
[69]Rao Dan,Qin Jianzhong,Tenger,et al.Source analysis of oil seepage and bitumen originating from marine layer strata in Guangyuan area,the northwest Sichuan Basin[J].Petroleum Geology & Experiment,2008,30(6):596-599,60.
饶丹,秦建中,腾格尔,等.川西北广元地区海相层系油苗和沥青来源分析[J].石油实验地质,2008,30(6):596-599,60.
[70]Liu Chun,Zhang Huiliang,Shen Anjiang,et al.Geochemistry characteristics and origin of the Devonian oil-sandstone in the northwest of Sichuan Basin[J].Acta Petrolei Sinica,2010,31(2):253-258.
刘春,张惠良,沈安江,等.川西北地区泥盆系油砂岩地球化学特征及成因[J].石油学报,2010,31(2):253-258.
[71]Hao Bin,Hu Suyun,Huang Shipeng,et al.Geochemical characteristics and its significance of reservoir bitumen of Longwangmiao Formation in Moxi area,Sichuan Basin[J].Geoscience,2016,30(3):614-626.
郝彬,胡素云,黄士鹏,等.四川盆地磨溪地区龙王庙组储层沥青的地球化学特征及其意义[J].现代地质,2016,30(3):614-626.
[72]Stahl W J,Carey B D.Source-rock identification by isotope analyses of natural gases from fields in the Val Verde and Delaware basins,West Texas[J].Chemical Geology,1975,16(4):257-267.
[73]Hu Anping.Organic Petrographic and Organic Geochemical Studies of the Sour Gas Accumulations in the Lower Triassic Feixianguan Formation,NE Sichuan Basin[D].Hangzhou:Zhejiang University,2009:145.
胡安平.川东北飞仙关组高含硫化氢气藏有机岩石学与有机地球化学研究[D].杭州:浙江大学,2009:145.
[74]Ni Yunyan,Liao Fengrong,Gong Deyu,et al.Stable carbon and hydrogen isotopic characteristics of natural gas from Taibei Sag,Turpan-Hami Basin[J].Petroleum Exploration and Development,2019,46(3):1-12.
倪云燕,廖凤蓉,龚德瑜,等.吐哈盆地台北凹陷天然气碳氢同位素组成特征[J].石油勘探与开发,2019,46(3):1-12.
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