收稿日期: 2017-04-10
修回日期: 2017-11-20
网络出版日期: 2018-02-10
基金资助
The analysis of helium accumulation conditions and prediction of helium resource in Weihe Basin
Received date: 2017-04-10
Revised date: 2017-11-20
Online published: 2018-02-10
渭河盆地氦气资源量在计算原理和参数选取上存在较大争议。据此,统计了渭河盆地101件油气井和地热井样品的气体成分和氦同位素数据,分析了该盆地的氦气成藏条件,并在综合选取和评估各项参数的基础上,估算了渭河盆地氦气资源量。结果表明,钻孔样品氦气体积分数平均为1.50%,最高达9.23%;氦源岩、地下水系统、载体气和断裂是氦气生成、运移和成藏的控制条件,其中盆地南缘花岗岩体和盆地内部隐伏磁性体是盆地最主要的氦源岩;根据盆地内地热流体储量、气水比、氦气体积分数估算出盆地内氦气资源量为21.30×108 m3;根据氦源岩有效面积、水循环深度、岩体密度、铀钍含量估算得出自花岗岩体形成、盆地断陷和储层形成后的生氦量分别为185.21×108 m3、37.58×108 m3和4.16×108 m3。综合认为渭河盆地的氦气资源勘探前景良好。
张文,李玉宏,王利,赵峰华,韩伟,宋昌贵 . 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 . DOI: 10.11764/j.issn.1672-1926.2017.12.002
There are dispute on the calculation principle and parameters selection of helium resource prediction in Weihe Basin.Here gas compositions and helium isotopes data of 101 oil & gas wells and geothermal wells in Weihe Basin were collected;helium accumulation conditions analyzed;the helium resources calculated on the basis of comprehensive selection and evaluation of various parameters.The results showed that the volume fraction of helium is 1.50% in average and 9.23% to maximum.Helium source rocks,groundwater systems,carrier gases and fractures are the control conditions of helium production,migration and accumulation,in which the granite body in southern margin of the basin and concealed magnetic body interior basin are most likely the helium source rocks.Evaluation of helium resources in Weihe Basin are as follows:(1)the helium resource is calculated to be 21.30×108 m3 on the basis of the geothermal fluid reserves,the gas-water ratio,the volume fraction of helium gas;(2)according to the effective area of the helium source rocks,water cycle depth,rock density,uranium and thorium concentrations,the helium quantities produced since the formation of granite rocks,depression of the basin and formation of reservoir are 185.21×108 m3,37.58×108 m3 and 4.16×108 m3respectively,showing the good helium resource prospect in Weihe Basin.
Key words: Weihe Basin; Helium; Accumulation conditions; Helium resource
[1]Mamyrin B A,Tolstikhin I N.Helium Isotopes in Nature[M].Amsterdam:Elsevier,1984.
[2]Tolstikhin I,Lehmann B E,Loosli H H,et al.Helium and argon isotopes in rocks,minerals,and related ground waters:A case study in northern Switzerland[J].Geochimica et Cosmochimica Acta,1996,60(9):1497-1514.
[3]Xu Yongchang.Helium isotope distribution of natural gasses and its structural setting[J].Earth Science Frontiers,1997,4(3/4):185-190.
徐永昌.天然气中氦同位素分布及构造环境[J].地学前缘,1997,4(3/4):185-190.
[4]Hu Ruizhong,Zhong Hong,Ye Zaojun,et al.Helium and argon isotopes geochemistry in Jinding super-large lead-zinc deposit[J].Chinese Science:Earth Science,1998,28(3):208-213.
胡瑞忠,钟宏,叶造军,等.金顶超大型铅锌矿床氦、氩同位素地球化学[J].中国科学:地球科学,1998,28(3):208-213.
[5]Fourré E,Jean-Baptiste P,Dapoigny A,et al.Dissolved helium distribution in the Oxfordian and Dogger deep aquifers of the Meuse/Haute-Marne area[J].Physics & Chemistry of the Earth Parts A/b/c,2011,36(17/18):1511-1520.
[6]Hamak J E.Mineral commodity summarises 2014,Helium[R].Washington D C:U.S.Geological Survey,2014:72-73.
[7]Hamak J E.Mineral Commodity Summarises 2016,Helium[R].Washington D C:U.S.Geological Survey,2016:78-79.
[8]Wang Peiye,Song Tao,Zhen Yunqin,et al.Sichuan Weiyuan Gasfield:A typical example for mantle-crust source[J].Contributions to Geology and Mineral Resource Research,2011,26(1):63-73.
王佩业,宋涛,真允庆,等.四川威远气田:幔壳混源成因的典型范例[J].地质找矿论丛,2011,26(1):63-73.
[9]Zhang Fuli,Sun Qibang,Wang Yunxing,et al.Evaluation of water soluble helium resources in Weihe Basin[J].Journal of Geomechanics,2012,18(2):195-202.
张福礼,孙启邦,王行运,等.渭河盆地水溶氦气资源评价[J].地质力学学报,2012,18(2):195-202.
[10]Li Yuhong,Wang Yunxing,Han Wei.Mode of occurrence of helium in Weihe Basin,Shaanxi Province and its significance[J].Geological Bulletin of China,2016,35(2/3):372-378.
李玉宏,王行运,韩伟.陕西渭河盆地氦气资源赋存状态及其意义[J].地质通报,2016,35(2/3):372-378.
[11]Liu Jianchao,Li Rongxi,Wei Gangfeng,et al.Origin and source of soluble helium gas in geothermal water,Weihe Basin[J].Geological Science and Technology Information,2009,28(6):84-88.
刘建朝,李荣西,魏刚峰,等.渭河盆地地热水水溶氦气成因与来源研究[J].地质科技情报,2009,28(6):84-88.
[12]Zhang Xun.Accumulation Conditions and Resource Prediction of Nature Gas and Helium Gas in Weihe Basin[D].Xi’an:Chang’an University,2015:102-119.
张雪.渭河盆地天然气及氦气成藏条件与资源量预测[D].西安:长安大学,2015:102-119.
[13]Li Yuhong,Lu Jincai,Li Jinchao,et al.Distribution of the helium-rich wells and helium derivation in Weihe Basin[J].Journal of Jilin University:Earth Science Edition,2011,41(S1):47-53.
李玉宏,卢进才,李金超,等.渭河盆地富氦天然气井分布特征与氦气成因[J].吉林大学学报:地球科学版,2011,41(S1):47-53.
[14]Zhang Mingsheng,Zhang Jingong,Zhang Jiankun,et al.The progress of helium accumulation[J].Ground Water,2014,36(3):189-191.
张明升,张金功,张建坤,等.氦气成藏研究进展[J].地下水,2014,36(3):189-191.
[15]Li Yuhong,Zhang Wen,Wang Li,et al.Henry’ Law and accumulation of crust-derived helium:A case from Weihe Basin,China[J].Natural Gas Geoscience,2017,28(4):495-501.
李玉宏,张文,王利,等.亨利定律与壳源氦气弱源成藏——以渭河盆地为例[J].天然气地球科学,2017,28(4):495-501.
[16]Brown A A.Origin of High Helium Concentrations in Dry Gas by Water Fractionation[C].AAPG Convention,Calgary,Calgary,Alberta,Canada,2005.
[17]Brown A A.Formation of High Helium Gases:A Guide for Explorationists[C].AAPG Convention,Louisianal,New Orleans,USA,2010.
[18]Han Wei,Li Yuhong,Lu Jincai,et al.The factors responsible for the unusual content of helium-rich natural gas in the Weihe Basin,Shaanixi Province[J].Geological Bulletin of China,2014,33(11):1836-1841.
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.
[19]Ballentine C J,Burnard P G.Production,release and transport of noble gases in the continental crust[J].Reviews in Mineralogy & Geochemistry,2002,47(1):481-538.
[20]Zhai Guangming,Wang Shenyan,Shi Xunzhi,et al.Petroleum Geology of China(Vol.12):Changqing Oilfield[M].Beijing:Petroleum Industry Press,1992:23-55.
翟光明,王慎言,史训知,等.中国石油地质志(卷12):长庆油田[M].北京:石油工业出版社,1992:23-55.
[21]Wang Jianqiang,Liu Chiyang,Gao Fei,et al.Pre-Cenozoic geological characteristics and oil-gas significance in Weihe Basin,Shaanxi Province[J].Geological Bulletin of China,2015,34(10):1981-1991.
王建强,刘池洋,高飞,等.陕西渭河盆地前新生界地质特征及其油气意义[J].地质通报,2015,34(10):1981-1991.
[22]Zhang Lin.Geothermal and Associated Water Soluble Gas Resources Exploration and Prospect Forecase of Weihe Basin[D].Xi’an:Chang’an University,2014:1-146.
张林.渭河盆地地热及伴生水溶气资源探索及远景预测[D].西安:长安大学,2014:1-146.
[23]Zhou Z,Ballentine C J.4He dating of groundwater associated with hydrocarbon reservoirs[J].Chemical Geology,2006,226(3/4):309-327.
[24]Kunz W,Schintlmeister J.Elements from Neutron to Magnesium[M].Oxford,London,Edinburgh,New York,Paris,Frankfurt:Pergamon Press,1965:171-222.
[25]Tissot B P,Welte D H.Petroleum Formation and Occurrence:A New Approach to Oil and Gas Exploration[M].Berlin,Heidelberg,New York,Tokyo:Springer Verlag,1984,1-538.
[26]Wang Jiangbo,Li Weihong,Lai Shaocong.Discussion on ore-control factors and mineralization of the Lantian Uranium field,Shaanxi[J].Northwestern Geology,2013,46(1):154-161.
王江波,李卫红,赖绍聪.陕西蓝田铀矿田控矿因素与成矿作用过程探讨[J].西北地质,2013,46(1):154-161.
[27]Li Yuhong,Wang Yunxing,Han Wei.Progress and achievements of helium gas resource survey in Weihe Basin[J].Geological Survey of China,2015,2(6):1-6.
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.
[28]Xu Qiulong,Zuo Ping.Helium measurement and its application in seismology[J].Earthquake Research in Plateau,1993,5(4):38-42.
许秋龙,左平.氦气测量及其在地震学中的应用[J].高原地震,1993,5(4):38-42.
[29]Kong Lingchang,Wang Guiqing,Wang Zhimin,et al.Study on relationship between abnormality of helium concentration and earthquakes in observation wells[J].Seismological and Geomagnetic Observation and Research,2007,28(6):32-36.
孔令昌,王桂清,王志敏,等.观测井中氦含量异常与地震关系的研究[J].地震地磁观测与研究,2007,28(6):32-36.
[30]Honda M,Kurita K,Hamano Y,et al.Experimental studies of He and Ar degassing during rock fracturing[J].Earth & Planetary Science Letters,1982,59(2):429-436.
[31]Pacheco N,Ali S F.Helium Resources of the United States-2007,Technical Note 429.Bureau of Land Management[C].Denver,Colorado,2008:1-19.
[32]Danabalan D,Gluyas J G,Macpherson,et al.New High-Grade Helium Discoveries in Tanzania[C].Goldschmidt Conference,Japan:Yokohama.2016.
[33]Jin Qinhai,Ju Dangchen.Genesis of Xiba compound rock mass in southern Taibai,Shaanxi and its relationship with Shuangwang gold deposit[J].Geoscience,1990,4(4):65-76.
金勤海,鞠党辰.陕西太白南部西坝复式岩体的成因及其与双王金矿床的关系[J].现代地质,1990,4(4):65-76.
[34]Zuo Wenqian,Sha Yazhou,Chen Bing,et al.U-Pb isotopic dating of zircon from Damaogou granite stock of Guangshigou uranium deposit in Danfeng area and it’s significance[J].Uranium Geology,2010,26(4):222-227.
左文乾,沙亚洲,陈冰,等.丹凤地区光石沟铀矿床大毛沟岩株锆石U-Pb同位素定年及其地质意义[J].铀矿地质,2010,26(4):222-227.
[35]Qi Qiuju,Wang Xiaoxia,Ke Changhui,et al.Geochronology and origin of the Laoniushan complex in the southern margin in North China Block and their implications:New evidences from zircon dating,Hf isotopes and geochemisty[J].Acta Petrologica Sinica,2012,28(1):279-301.
齐秋菊,王晓霞,柯昌辉,等.华北地块南缘老牛山杂岩体时代、成因及地质意义——锆石年龄、Hf同位素和地球化学新证据[J].岩石学报,2012,28(1):279-301.
[36]Guo Bo,Zhu Laimin,Li Ben,et al.Zircon U-Pb age and Hf isotope composition of the Huashan and Heyu granite plutons at the southern margin of North China Craton:Implication for geodynamic setting[J].Acta Petrologica Sinica,2009,25(2):265-281.
郭波,朱赖民,李犇,等.华北陆块南缘华山和合峪花岗岩岩体锆石U-Pb年龄、Hf同位素组成与成岩动力学背景[J].岩石学报,2009,25(2):265-281.
[37]Yan Zhen.Granite in Shaanxi Province[M].Xi’an:Xi’an Jiaotong University Press,1985:1-321.
严阵.陕西省花岗岩[M].西安:西安交通大学出版社,1985:1-321.
[38]Ren Juan.Probe on the Deep Crustal Structure in Weihe Basin and Tectonics Research of Basin[D].Xi’an:Chang’an University,2012:1-251.
任隽.渭河盆地深部地壳结构探测与盆地构造研究[D].西安:长安大学,2012:1-251.
[39]Wang Wanhong,Zhang Hui,Su Hejun.Research on the relation of circulation depth of hot spring water with seismicity in the northern margin fault zone of Qinling[J].Northwestern Seismological Journal,2008,30(1):36-41.
汪万红,张慧,苏鹤军.秦岭北缘断裂带温泉水循环深度与地震活动性的关系研究[J].西北地震学报,2008,30(1):36-41.
[40]Holland G,Lollar B S,Li L,et al.Deep fracture fluids isolated in the crust since the Precambrian Era.[J].Nature,2013,497(7449):357-60.
/
| 〈 |
|
〉 |