Natural Gas Geoscience ›› 2020, Vol. 31 ›› Issue (11): 1585-1592.doi: 10.11764/j.issn.1672-1926.2020.03.014

Previous Articles     Next Articles

Finding of the Dongping economic Helium gas field in the Qaidam Basin, and Helium source and exploration prospect

Xiao-bao ZHANG1,2,3(),Fei ZHOU3,Zhan-yuan CAO1,2,3,Ming-liang LIANG4   

  1. 1.Petroleum Resources Research Center,Northwest Institute of Eco?Environments and Resources,CAS,Lanzhou 730000,China
    2.Key Laboratory of Petroleum Resources Research,Gansu Province,Lanzhou 730000,China
    3.Qinghai Oil Field Company,CNPC,Dunhuang 736202,China
    4.China Academy of Geological Sciences,Institute of Geomechanics,Beijing 100081,China
  • Received:2020-02-17 Revised:2020-03-23 Online:2020-11-10 Published:2020-11-24

Abstract:

In order to further clarify the distribution of Helium resources in Qaidam Basin, the geochemical characteristics of natural gas in Dongping and other gas fields were analyzed. The results show that the Helium content of 21 natural gas samples from Dongping 1, Dongping 3 well areas in Dongping Gas Field and Jiantan 1 well area in Jiandingshan Gas Field is more than 0.05%, reaching an economic level, which has a minimum value of 0.07%, a maximum of 1.069%, and an average of 0.386%, therefore the economic Helium fields were found in the basin. The minimum 3He/4He of the Dongping Gas Field and its neighboring Niudong Gas Field is 1.01×10-8, the maximum is 3.62×10-8 and the average is 1.86×10-8, in an order of 1.86×10-8, showing a crust-sourced origin. A comprehensive analysis exhibits that the economic helium fields are sourced from the granite and granitic gneiss base. The granite and granitic gneiss base in the basin is widely distributed, which means the exploration prospect is very broad.

Key words: Economic helium gas field, Crust source, Granitic base, Dongping Gas Field, Qaidam BasinFoundation Items: The General Program of Natural Science Foundation of China (Grand No. 41972135), The Youth Program of Natural Science Foundation of China (Grand No. 41702150)

CLC Number: 

  • TE122.1
1 徐永昌,沈平,陶明信,等.东部油气区天然气中幔源挥发份的地球化学——Ⅰ.氦资源的新类型:沉积壳层幔源氦的工业储集[J].中国科学:D 辑,1996,26(1):1-8.
XU Y C, SHEN P, TAO M X, et al. Geochemistry of mantle-derived volatiles in the oil-gas area:Ⅰ. A new type of helium resources: Industrial reservoir of moutle derived helium from sedimentary crust[J]. Science in China:Series D, 1996, 26(1):1-8.
2 王熙庭, 任庆生. 氦资源、 应用、 市场和提取技术[J]. 天然气化工,2012,37(1):73-78.
WANG X T, REN Q S. Resources, application, market and extraction technologies of Helium[J].Natural Gas Chemical Industry, 2012, 37(1):73-78.
3 凌辉,周勇义,张黎伟,等. 氦资源对科学仪器及科研项目的影响与对策[J].科学管理研究,2012,30(6):21-24.
LIN H,ZHOU Y Y, ZHANG L W, et al. The affect of Helium resources to scientific instruments and scientific programs[J].Scientific Administration and Research,2012,30(6):21-24.
4 徐永昌,沈平,李玉成.中国最古老的气藏——四川威远震旦纪气藏[J].沉积学报,1989,7(4):3-13.
XU Y C, SHEN P, LI Y C. The oldest gas pool of China—Weiyuan Sinian gas pool, Sichuan Province[J]. Acta Sedimentologica Sinica, 1989, 7(4):3-13.
5 戴金星. 威远气田成藏期及气源[J]. 石油实验地质, 2003,25(5);473-480.
DAI J X. Pool-forming periods and gas sources of Weiyuan Gasfield[J]. Petroleum Geology & Experiment, 2003,25(5):473-480.
6 郭念发,尤孝忠,徐俊.苏北盆地溪桥含氦天然气田地质特征及含氦天然气勘探前景[J].石油勘探与开发,1999,26(5):24-26.
GUO N F, YOU X Z, XU J. Geological character of Xiqiao Helium-bearing gas field and prospecting of Helium-bearing natural gas in North Jiangsu Basin[J]. Petroleum Exploration and Development , 1999, 26(5): 24-26.
7 李海庆.江苏黄桥 CO2气田成藏条件研究及意义[J].能源技术与管理,2012(1):128-130.
LI H Q. Research and significance of reservoir forming conditions of Huangqiao CO2 gas field, Jiangsu Province[J]. Energy Technology and Management, 2012 (1):128-130.
8 徐永昌,沈平,陶明信,等.幔源氦的工业储聚和郯庐大断裂带[J].科学通报,1990(12):932-935.
XU Y C, SHEN P, TAO M X, et al. Industrial accumulation of slow source Helium and Tanlu fault zone[J].Chinese Science Bulletin, 1990 (12):932-935.
9 余琪祥,史政,王登高,等.塔里木盆地西北部氦气富集特征与成藏条件分析[J].西北地质,2013,46(4):215-222.
YU Q X, SHI Z, WANG D G, et al. Analysis on Helium enrichment characteristics and reservoir forming conditions in northwestern Tarim Basin[J].Northwestern Geology,2013,46 (4):215-222.
10 卢进才,魏仙样,李玉宏,等. 汾渭盆地富氦天然气成因及成藏条件初探[J].西北地质,2005,38(3):82-86.
LU J C, WEI X X, LI Y H, et al. Preliminary study about genesis and pool formation conditions of rich-Helium type natural gas[J].Northwestern Geology, 2005,38 (3):82-86.
韩伟,李玉宏,卢进才,等.陕西渭河盆地富氦天然气异常的影响因素[J].地质通报,2014,33(11):1836-1841.
HAN W, LI Y H, LU J C, et al. The factors responsible for the unusual content of Helium-rich natural gas in the Weihe Basin, Shaanxi Province[J]. Geological Bulletin of China, 2014, 33(11):1836-1841.
12 李玉宏,王行运,韩伟.渭河盆地氦气资源远景调查进展与成果[J].中国地质调查,2015,2(6):1-6.
LI Y H, WANG X Y, HAN W. Progress and results of investigations of Helium resources prospects in the Weihe Basin[J].Chinese Geological Investigation, 2015,2(6):1-6.
13 张文,李玉宏,王利,等.渭河盆地氦气成藏条件分析及资源量预测[J].天然气地球科学,2018,29(2):236-244.
ZHANG W, LI Y H, WANG L, et al. Resource prediction and pool-forming conditions of Helium gas in the Weihe Basin[J].Natural Gas Geoscience, 2018, 29(2):236-244.
14 陶小晚,李建忠,赵力彬,等. 我国氦气资源现状及首个特大型富氦储量的发现:和田河气田[J].地球科学,2019,44(3):1024-1041.
TAO X W, LI J Z, ZHAO L B, et al. Finding of the first very large Helium-rich reserves: Hetianhe Gas Field and recent situation of Helium resources in China[J].Earth Sciences, 2019, 44(3):1024-1041.
15 张云鹏,李玉宏,卢进才,等.柴达木盆地北缘富氦天然气的发现——兼议成藏地质条件[J].地质通报,2016,35(2-3):364-371.
ZHANG Y P, LI Y H, LU J C, et al. Finding of Helium-rich natural gas in the north margin of the Qaidam Basin: Discussing the pool-forming geological conditions[J].Geological Bulletin, 2016,35(2-3):364-371.
16 杨振宁,李永红,刘文进,等.柴达木盆地北缘全吉山地区氦气形成地质条件及资源远 景分析[J].中国煤炭地质,2018,30(6):64-70.
YANG Z N, LI Y H, LIU W J, et al. Resources prospects and Helium-forming conditions in Quanjishan area in the north margin of the Qaidam Basin[J].China Coal Geology, 2018,30(6):64-70.
17 中国石油青海油田研究院天然气室. 天然气勘探部署[R]//2017勘探年会.敦煌:中国石油青海油田勘探开发研究院,2017.
Natural Gas Division, Research Institute of PetroChina Qinghai Oilfield Company. Natural Gas Exploration Deployment[R]. 2017 Anunal Exploration Meeting. Dunhuang: Petroleum Exploration and Development Institute, Qinghai Oilfield Company, CNPC, 2017.
18 张永庶,赖绍聪,巨银娟,等.东坪地区基岩测年研究[R].敦煌:中国石油青海油田勘探开发研究院,2017.
ZHANG Y S, LAI S C, JU Y J. Base Aging in the Dongping Area[R].Dunhuang: Petroleum Exploration and Development Institute, Qinghai Oilfield Company, CNPC, 2017.
19 徐永昌,沈平,刘文汇,等.天然气中稀有气体地球化学[M].北京:科学出版社,1998.
XU Y C, SHEN P, LIU W H, et al. Noble Gas Geochemistry in Natural Gases[M]. Beijing: Science Press,1998.
20 曹春辉,李中平,杜丽,等.气体同位素质谱仪MTA271分析天然气组分的方法研究[J].现代科学仪器,2011(5):103-106.
CAO C H, LI Z P, DU L, et al. Research of method of analyzing natural gas composition by a MAT271 mass spectrometer[J].Modern Scientific Instrument, 2011(5): 103-106.
21 周飞,张永庶,王彩霞,等. 柴达木盆地东坪—牛东地区天然气地球化学特征及来源探讨[J].天然气地球科学,2016,27(7):1312-1323.
ZHOU F, ZHANG Y S, WANG C X, et al. Geochemical characteristics and origin of natural gas in Dongping-Niudong area, Qaidam Basin,China[J].Natural Gas Geoscience, 2016,27(7):1312-1323.
22 POREDA R J, JENDEN P D, KAPLAN I R, et al. Mantle Helium in Sacramento Basin natural gas wells[J].Geochimica et Cosmochimica Acta, 1986, 50(12):2847-2853.
23 GOLD T, HELD M. Helium-nitrogen-methane systematics in natural gases of Texas and Kansas[J].Journal of Petroleum Geology, 1987,10(4): 415-424.
24 JENDEN P D, KAPLAN I R, POREDA R J. Origin of nitrogen-rich natural gases in the California great valley:Evidence from Helium, carbon an nitrogen isotope ratios[J]. Geochimica et Cosmochimica Acta, 1988,52(2): 851-861.
25 徐永昌,沈平,陶明信,等. 中国含油气盆地天然气中氦同位素分布[J].科学通报,1994,9(16):1505-1508.
XU Y C, SHEN P, TAO M X, et al. Distribution of Helium isotopes in natural gas of petroliferous basins in China[J]. Chinese Science Bulletin, 1994, 9 (16): 1505-1508.
26 徐永昌.天然气中的幔源稀有气体[J].地学前缘,1996,3(3-4):63-71.
XU Y C. The mantle noble gas of natural gases[J]. Earth Science Frontiers, 1996,3(3-4):63-71.
27 CHRISTIANSEN R L. Approximate distributions of major tectonic, sedimentary and igneous features in the US Cordilleran region during several post-Laramide time periods[C]// BURCHFIEL B C, LIPMAN P W, ZOBACH M L. The Cordilleran Orogen: Conterminous US: The Geology of North America. DNAG Vol. G-3.
Boulder, Colorado: Geological Society of America,1992.
28 BROWN A A. Formation of High Helium Gases: A Guide for Explorationists[C]. AAPG Convention, New Orleans, Louisiana, April11-14, 2010.
[1] Wei HAN, Wen-jin LIU, Yu-hong LI, Jun-lin ZHOU, Wen ZHANG, Yun-peng ZHANG, Xiao-hong CHEN, Bin HUANG. Characteristics of rare gas isotopes and main controlling factors of radon enrichment in the northern margin of Qaidam Basin [J]. Natural Gas Geoscience, 2020, 31(3): 385-392.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] LI Feng-jie~1,2,WANG Duo-yun~1. THE HIGH-RESOLUTION SEQUENCE STRATIGRAPHIC FEATURE OF YANCHANG FORMATION IN XIFENG OILFIELD, ORDOS BASIN[J]. Natural Gas Geoscience, 2006, 17(3): 339 -344 .
[2] Yan Cun-feng,Yuan Jian-ying,Zhao Ying-cheng,Wei Dong-tao,Li Zai-guang. JURASSIC SPORA POLLEN ASSEMBLAGES AND PALEOCLAMATE IN INNERMONGOLIA, GANSU, QINGHAI, CHINA[J]. Natural Gas Geoscience, 2006, 17(5): 634 -639 .
[3] . [J]. Natural Gas Geoscience, 1997, 8(2): 39 -41 .
[4] LI Guang-zhi, HU Bin, DENG Tian-long,YUAN Zi-yan . Petroleum Geological Significance of Microelements V and Ni[J]. Natural Gas Geoscience, 2008, 19(1): 13 -17 .
[5] . EVALUATING ON HYDROCARBON EXPLORATION POTENTIAL OF LOWER TERTIARY IN BODONG DEPRESSION BY BASIN MODELLING TECHNIQUE[J]. Natural Gas Geoscience, 2004, 15(4): 379 -382 .
[6] . THE KIND OF DINA 2 GAS FIELD[J]. Natural Gas Geoscience, 2004, 15(1): 91 -94 .
[7] QIN Bai-ping,Lü Xiu-xing,ZHANG Zhen-hong,WAN Xiao-long. NUMERICAL SIMULATION STUDY AND DEVELOPMENT MEANING OF CHANG 1 RESERVOIR IN DING 31 WELL AREA OFYOUFANGZHUANG OIL FIELD IN ORDOS BASIN[J]. Natural Gas Geoscience, 2004, 15(5): 531 -535 .
[8] . [J]. Natural Gas Geoscience, 1997, 8(5-6): 32 -36 .
[9] . [J]. Natural Gas Geoscience, 2002, 13(3-4): 45 -51 .
[10] . STUDYING ON BASIC THEORY AND INFLUENCE FACTOR OF GAS STORAGE IN S ALT CAVERNS BUILDING WITH WATER SOLUTION[J]. Natural Gas Geoscience, 2006, 17(2): 261 -266 .