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[1]李进步*,刘志军,张 晨,等.鄂尔多斯盆地靖边地区马家沟组气田水地球化学特征及锂来源[J].地球科学与环境学报,2024,46(05):651-662.[doi:10.19814/j.jese.2024.03023]
　LI Jin-bu*,LIU Zhi-jun,ZHANG Chen,et al.Geochemical Characteristics of Gas Field Water and Sources of Lithium from Majiagou Formation in Jingbian Area of Ordos Basin, China[J].Journal of Earth Sciences and Environment,2024,46(05):651-662.[doi:10.19814/j.jese.2024.03023]
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第46卷
期数:
2024年第05期
页码:
651-662
栏目:
沉积地质与油气勘探
出版日期:
2024-09-30

文章信息/Info

Title:
Geochemical Characteristics of Gas Field Water and Sources of Lithium from Majiagou Formation in Jingbian Area of Ordos Basin, China
文章编号:
1672-6561(2024)05-0651-12
作者:
李进步1*; 刘志军1; 张 晨1; 王昌勇2; 3; 谈曜杰2; 3; 钟良才2; 3; 朱梦悦2; 3
(1. 中国石油长庆油田分公司勘探开发研究院,陕西 西安 710018; 2. 成都理工大学 沉积地质研究院,四川 成都 610059; 3. 成都理工大学 自然资源部深时地理环境重建与应用重点实验室,四川 成都 610059)
Author(s):
LI Jin-bu1*;  LIU Zhi-jun1;  ZHANG Chen1;  WANG Chang-yong2; 3;  TAN Yao-jie2; 3; ZHONG Liang-cai2; 3;  ZHU Meng-yue2; 3
(1. Research Institute of Exploration and Development, Changqing Oilfield Company, PetroChina,Xi'an 710018, Shaanxi, China; 2. Institute ofSedimentary Geology, Chengdu University ofTechnology, Chengdu 610059, Sichuan, China; 3. Key Laboratory of Deep-time Geography and EnvironmentReconstruction andApplications ofMinistry ofNatural Resources, Chengdu University of Technology, Chengdu 610059, Sichuan, China)
关键词:
气田水;  锂;  矿化度;  化学系数;  同位素;  物质来源;  靖边地区;  鄂尔多斯盆地
Keywords:
gas field water;  lithium;  salinity degree;  chemical coefficient;  isotope;  material source;  Jingbian area;  Ordos Basin
分类号:
P618.13; TE133
DOI:
10.19814/j.jese.2024.03023
文献标志码:
A
摘要:
鄂尔多斯盆地靖边地区马家沟组气田水中Li+浓度较高,部分井区达到工业品位,勘探开发潜力巨大,但锂来源尚不明确。以靖边地区马家沟组气田水为研究对象,采用薄片鉴定、X射线衍射分析、微量元素分析及Sr、Li同位素分析等方法,对马家沟组气田水地球化学特征进行了研究,并讨论了水体中锂来源。结果表明:①气田水中离子浓度变化极大,矿化度为0.12～228.19 g·L-1,平均值为39.87 g·L-1,部分水体达到卤水范畴,气田水pH值为4.82～8.44,以弱酸性为主,水化学类型以CaCl2型为主,部分井区为MgCl2型或NaHCO3型; ②气田水钠氯系数普遍大于0.87,脱硫系数普遍小于1,变质系数普遍大于0,氯镁系数主要为20～90,储层整体封闭性好,水体还原性强,变质程度高,属于高变质、高浓缩的水体,部分井区储层封闭条件被破坏,受大气水影响明显; ③气田水Li同位素具有早奥陶世海水的特征,Sr同位素受到凝灰质组分及大气水岩溶的影响,87Sr/86Sr值高于马家沟组沉积时期正常海水; ④马家沟组含凝灰质组分的岩石和岩溶角砾岩填隙物普遍具有较高的Li+浓度,Li同位素特征指示气田水中锂主要来自马家沟组地层,马家沟组富锂气田水是加里东期马家沟组地下岩溶水埋藏和演化的结果。
Abstract:
The gas field water of Majiagou Famation in Jingbian area of Ordos Basin has a high Li+concentration, the lithium insome gas fieldwaterhas reached industrial grade with great potential for development. However, the sources of lithium from the gas field water is still unclear. According to thin section identification,X-ray diffraction analysis,trace element analysis, Sr and Li isotope analysis, the geochemical characteristics of gas field water in Majiagou Formation and the sources oflithium were studied. The results show that① the ion concentrationin the gas field water variesgreatly, and the salinitydegreeranges from 0.12 to 228.19 g·L-1 with an average of 39.87 g·L-1; partial water bodies reach the category of brine,and the pH value ranges from 4.82 to 8.44,mainly weakly acidic; the hydrochemical type is mainly CaCl2-type while some wells are MgCl2-type or NaHCO3-type.② The sodio-chlorine coefficient of gas field water is generally greater than 0.87, the desulfurization coefficient is generally less than 1, the metamorphism coefficient is generally greater than 0, and the chloro-magnesium coefficient mainly ranges from 20 to 90; the reservoir as a whole has a good sealing property, the water has a strong reducibility and high degree of metamorphism, which belongs to the high metamorphism and concentration water body; the sealing condition of reservoir in some wells is damaged andobviously affected by atmospheric water.③ The Li isotope of gas field water has the characteristics of Early Ordovician sea water, while the Sr isotope is affected by the tuff compositions as well as the karst of atmospheric water, and the 87Sr/86Sr value is higher than that of the normal sea water in the sedimentary period of Majiagou Formation.④The tuffaceous rocks and karst breccia interstitial material of Majiagou Formation generally have high Li+concentration. Li isotopic characteristics indicate that Li+ in gas field water mainly comes from Majiagou Formation, the Li-rich gas field water is the results of burial and evolution of underground karst water of Caledonian in Majiagou Formation.

参考文献/References:

[1] 王登红.关键矿产的研究意义、矿种厘定、资源属性、找矿进展、存在问题及主攻方向[J].地质学报,2019,93(6):1189-1209.
WANG Deng-hong.Study on Critical Mineral Resources:Significance of Research,Determination of Types,Attributes of Resources,Progress of Prospecting,Problems of Utilization,and Direction of Exploitation[J].Acta Geologica Sinica,2019,93(6):1189-1209.
[2]王秋舒,元春华.全球锂矿供应形势及我国资源安全保障建议[J].中国矿业,2019,28(5):1-6.
WANG Qiu-shu,YUAN Chun-hua.The Global Supply Situation of Lithium Ore and Suggestions on Resources Security in China[J].China Mining Magazine,2019,28(5):1-6.
[3]陈 瑜,徐 飞,程宏飞,等.锂同位素地球化学研究新进展[J].地学前缘,2023,30(5):469-490.
CHEN Yu,XU Fei,CHENG Hong-fei,et al.Lithium Isotope Geochemistry:A Review[J].Earth Science Frontiers,2023,30(5):469-490.
[4]毛景文,杨宗喜,谢桂青,等.关键矿产:国际动向与思考[J].矿床地质,2019,38(4):689-698.
MAO Jing-wen,YANG Zong-xi,XIE Gui-qing,et al.Critical Minerals:International Trends and Thinking[J].Mineral Deposits,2019,38(4):689-698.
[5]翟明国,吴福元,胡瑞忠,等.战略性关键金属矿产资源:现状与问题[J].中国科学基金,2019,33(2):106-111.
ZHAI Ming-guo,WU Fu-yuan,HU Rui-zhong,et al.Critical Metal Mineral Resources:Current Research Status and Scientific Issues[J].Bulletin of National Natural Science Foundation of China,2019,33(2):106-111.
[6]GOURCEROL B,GLOAGUEN E,MELLETON J,et al.Re-assessing the European Lithium Resource Potential:A Review of Hard-rock Resources and Metallogeny[J].Ore Geology Reviews,2019,109:494-519.
[7]刘 学,郑军卫,刘文浩,等.非常规卤水型锂资源开发现状与研究进展[J].矿产综合利用,2024,45(4):21-26,56.
LIU Xue,ZHENG Jun-wei,LIU Wen-hao,et al.Development Status and Research Progress of Unconventional Brine-type Lithium Resources[J].Multipurpose Utilization of Mineral Resources,2024,45(4):21-26,56.
[8]魏江桥,王安建,马 哲,等.锂资源全球治理体系历史演变、现实困境与中国参与策略[J].科技导报,2024,42(5):81-91.
WEI Jiang-qiao,WANG An-jian,MA Zhe,et al.Historical Evolution,Current Status,Realistic Challenges,and China's Strategy of the Global Governance System of Lithium Resources[J].Science & Technology Review,2024,42(5):81-91.
[9]赵俊兴,刘小驰.青藏高原锂资源成岩-成矿作用研究进展:前言[J].岩石学报,2024,40(2):339-346.
ZHAO Jun-xing,LIU Xiao-chi.Research Progress of Petrogenesis-mineralization in the Lithium Resources on the Tibetan Plateau:Preface[J].Acta Petrologica Sinica,2024,40(2):339-346.
[10]翟明国,胡 波.矿产资源国家安全、国际争夺与国家战略之思考[J].地球科学与环境学报,2021,43(1):1-11.
ZHAI Ming-guo,HU Bo.Thinking to State Security,International Competition and National Strategy of Mineral Resources[J].Journal of Earth Sciences and Environment,2021,43(1):1-11.
[11]张英利,陈 雷,王坤明,等.豫西巩义地区上石炭统本溪组泥岩地球化学和富锂特征及其控制因素[J].地球科学与环境学报,2023,45(2):208-226.
ZHANG Ying-li,CHEN Lei,WANG Kun-ming,et al.Geochemistry and Li-rich Characteristics of Mudstones from Upper Carboniferous Benxi Formation in Gongyi Area,the Western Henan, China and Their Controlling Factors[J].Journal of Earth Sciences and Environment,2023,45(2):208-226.
[12]BRADLEY D C,STILLING L L,JASKULA B W,et al.Lithium[C]∥SCHULZ K J,DEYOUNG J H,SEAL II R R,et al.Critical Mineral Resources of the United States:Economic and Environmental Geology and Prospects for Future Supply.Reston:USGS,2017:1802-K.
[13]孟军海,林佳富,才智杰,等.柴达木盆地盐湖型锂矿床地质特征与地球物理探测[J].地球科学与环境学报,2022,44(1):124-131.
MENG Jun-hai,LIN Jia-fu,CAI Zhi-jie,et al.Geologi-cal Characteristics and Geophysical Exploration of Salt Lake-type Lithium Deposits in Qaidam Basin,China[J].Journal of Earth Sciences and Environment,2022,44(1):124-131.
[14]高娟琴,王登红,王 伟,等.国内外主要油(气)田水中锂提取现状及展望[J].地质学报,2019,93(6):1489-1500.
GAO Juan-qin,WANG Deng-hong,WANG Wei,et al.Current Status and Prospects of Lithium Extraction in Major Domestic and Foreign Oil(Gas)Field Waters[J].Acta Geologica Sinica,2019,93(6):1489-1500.
[15]许建新,秦成功,韩积斌,等.锂元素及其同位素对南翼山油田卤水形成演化的指示意义[J].盐湖研究,2023,31(1):11-24.
XU Jian-xin,QIN Cheng-gong,HAN Ji-bin,et al.Geo-chemistry of Li and Its Isotope:Implications for Origin and Evolution of Oilfield Water in Nanyishan Tectonic Area,Qaidam Basin,Northwest China[J].Journal of Salt Lake Research,2023,31(1):11-24.
[16]韩佳欢,郑绵平,乜 贞,等.我国深层地下卤水钾、锂资源及其开发前景[J].盐湖研究,2024,32(2):90-100.
HAN Jia-huan,ZHENG Mian-ping,NIE Zhen,et al.Lithium and Potassium Resources of Oilfield Brine and Development Prospects in China[J].Journal of Salt Lake Research,2024,32(2):90-100.
[17]高娟琴,于 扬,仲佳爱,等.川东北黄金口背斜ZK001钻孔流体地球化学及含锂特征[J].地球科学与环境学报,2019,41(2):197-208.
GAO Juan-qin,YU Yang,ZHONG Jia-ai,et al.Geochemical and Li-bearing Characteristics of Fluids from Borehole ZK001 in Huangjinkou Anticline of the Northeastern Sichuan,China[J].Journal of Earth Sciences and Environment,2019,41(2):197-208.
[18]于升松.湖北江汉盆地潜江凹陷深层地下卤水水文地球化学研究[J].盐湖研究,1994,2(1):6-17.
YU Sheng-song.The Hydrochemical Characteristics of the Deep Brines in Basin Q,Hubei Province[J].Journal of Salt Lake Science,1994,2(1):6-17.
[19]赖 锦,刘秉昌,冯庆付,等.鄂尔多斯盆地靖边气田马家沟组五段白云岩沉积微相测井识别与评价[J].地质学报,2020,94(5):1551-1567.
LAI Jin,LIU Bing-chang,FENG Qing-fu,et al.Well Logging Identification and Evaluation of Depositional Microfacies in Dolostones from the 5th Member of the Ordovician Majiagou Formation in the Jingbian Gas Field,Ordos Basin[J].Acta Geologica Sinica,2020,94(5):1551-1567.
[20]何 江,冯春强,马 岚,等.风化壳古岩溶型碳酸盐岩储层成岩作用与成岩相[J].石油实验地质,2015,37(1):8-16.
HE Jiang,FENG Chun-qiang,MA Lan,et al.Diagene-sis and Diagenetic Facies of Crust-weathered Ancient Karst Carbonate Reservoirs[J].Petroleum Geology & Experiment,2015,37(1):8-16.
[21]牟春国,许 杰,古永红,等.鄂尔多斯盆地中东部奥陶系马家沟组四段储层特征及主控因素[J].石油实验地质,2023,45(4):780-790.
MOU Chun-guo,XU Jie,GU Yong-hong,et al.Reservoir Characteristics and Main Controlling Factors of the Fourth Member of Ordovician Majiagou Formation in the Central and Eastern Ordos Basin[J].Petroleum Geology & Experiment,2023,45(4):780-790.
[22]苏嫒娜,田世洪,李真真,等.MC-ICP-MS高精度测定Li同位素分析方法[J].地学前缘,2011,18(2):304-314.
SU Ai-na,TIAN Shi-hong,LI Zhen-zhen,et al.High-precision Measurement of Lithium Isotopes Using MC-ICP-MS[J].Earth Science Frontiers,2011,18(2):304-314.
[23]杨仁超,董 亮,张 吉,等.苏里格气田西区地层水成因、分布规律与控制因素[J].沉积学报,2022,40(1):267-280.
YANG Ren-chao,DONG Liang,ZHANG Ji,et al.Ori-gin,Distribution and Controlling Factors of Stratigraphic Water in the Western Sulige Gas Field[J].Acta Sedimentologica Sinica,2022,40(1):267-280.
[24]蔡立国,钱一雄,刘光祥,等.塔河油田及邻区地层水成因探讨[J].石油实验地质,2002,24(1):57-60.
CAI Li-guo,QIAN Yi-xiong,LIU Guang-xiang,et al.Origin of Formation Water in Tahe Oilfield and Adjacents[J].Petroleum Geology & Experiment,2002,24(1):57-60.
[25]满红梅,叶加仁,李令喜,等.东濮凹陷西部斜坡带油田水特征及其油气地质意义[J].地质科技情报,2009,28(3):67-72.
MAN Hong-mei,YE Jia-ren,LI Ling-xi,et al.Characteristics of Oilfield Water and Its Implications to Petroleum Geology in the Western Slope Belt,Dongpu Depression[J].Geological Science and Technology Information,2009,28(3):67-72.
[26]魏 丽.靖边潜台西北侧马五段碳酸盐岩古岩溶储层的形成与天然气成藏规律[D].西安:西北大学,2016.
WEI Li.The Formation of Carbonate Ancient Karst Reservoir Rock and The Hydrocarbon Accumulation Rule in Ma5 Member,the Northwestern Jingbian Bu-ried Platform[D].Xi'an:Northwest University,2016.
[27]张汪明,曾溅辉,李 飞,等.柴西地区古近系和新近系地层水化学特征及其成因[J].地球科学与环境学报,2016,38(4):558-568.
ZHANG Wang-ming,ZENG Jian-hui,LI Fei,et al.Hydrochemistry Characteristics and Origin of Formation Water of Paleogene and Neogene in the Western Qaidam Basin[J].Journal of Earth Sciences and Environment,2016,38(4):558-568.
[28]李建森,李廷伟,马海州,等.柴达木盆地西部新近系和古近系油田卤水水化学特征及其地质意义[J].水文地质工程地质,2013,40(6):28-36.
LI Jian-sen,LI Ting-wei,MA Hai-zhou,et al.Investigation of the Chemical Characteristics and Its Geological Significance of the Tertiary Oilfield Brine in the Western Qaidam Basin[J].Hydrogeology & Engineering Geology,2013,40(6):28-36.
[29]曹 琴,周 训,张 欢,等.四川盆地卧龙河储卤构造地下卤水的水化学特征及成因[J].地质通报,2015,34(5):990-997.
CAO Qin,ZHOU Xun,ZHANG Huan,et al.Hydrochemical Characteristics and Genesis of the Subsurface Brines in the Wolonghe Brine-bearing Structure of Sichuan Basin[J].Geological Bulletin of China,2015,34(5):990-997.
[30]韩 光,樊启顺,刘久波,等.柴达木盆地中西部背斜构造深层卤水水化学特征与成因[J].盐湖研究,2021,29(4):1-11.
HAN Guang,FAN Qi-shun,LIU Jiu-bo,et al.Origin and Hydrochemistry of Deep Brines from Anticlinal Reservoir in the Western-central Qaidam Basin[J].Journal of Salt Lake Research,2021,29(4):1-11.
[31]查 明,陈中红.山东东营凹陷前古近系水化学场、水动力场与油气成藏[J].现代地质,2008,22(4):567-575.
ZHA Ming,CHEN Zhong-hong.Formation Water Chemical and Hydrodynamic Fields and Their Relations to the Hydrocarbon Accumulation in the Pre-Tertiary of Dongying Depression,Shandong[J].Geoscience,2008,22(4):567-575.
[32]李雯霞,张西营,苗卫良,等.柴达木盆地北缘冷湖三号构造油田水水化学特征[J].盐湖研究,2016,24(2):12-18.
LI Wen-xia,ZHANG Xi-ying,MIAO Wei-liang,et al.Hydrochemical Charateristics of Oilfield Waters in Lenghu No.3 Structure Area of North Edge of Qai-dam Basin[J].Journal of Salt Lake Research,2016,24(2):12-18.
[33]李 阳.东胜气田锦66井区盒2+3段地层水特征及地质意义[J].石油地质与工程,2019,33(2):59-63.
LI Yang.Characteristics and Geological Significance of the Formation Water for 2+3th Member of Xiashihezi Formation in Jin 66 Well Block of Dongsheng Gas Field[J].Petroleum Geology and Engineering,2019,33(2):59-63.
[34]贾存善,马旭杰,饶 丹,等.塔河油田奥陶系油田水同位素特征及地质意义[J].石油实验地质,2007,29(3):292-297.
JIA Cun-shan,MA Xu-jie,RAO Dan,et al.Isotopic Characteristics of Oil Field Waters from Ordovician Oil Accumulations in Tahe Oilfield and Its Geological Significances[J].Petroleum Geology & Experiment,2007,29(3):292-297.
[35]余小灿,刘成林,王春连.锂同位素地球化学在大陆地热体系研究中的应用[J].地球科学进展,2020,35(3):246-258.
YU Xiao-can,LIU Cheng-lin,WANG Chun-lian.Application of Lithium Isotope Geochemistry to the Study of the Continental Geothermal System[J].Advances in Earth Science,2020,35(3):246-258.
[36]庄思蝶,周晓成,李鹏飞,等.新疆塔什库尔干断裂带温泉环境地球化学特征[J].地球科学与环境学报,2022,44(4):699-712.
ZHUANG Si-die,ZHOU Xiao-cheng,LI Peng-fei,et al.Environmental Hydrogeochemical Characteristics of Hot Springs in Tashkurgan Fault Zone of Xinjiang,China[J].Journal of Earth Sciences and Environment,2022,44(4):699-712.
[37]于 沨,于 扬,王登红,等.锂同位素地球化学在地热流体水岩反应中的应用:以川西现代富锂热泉研究为例[J].岩石学报,2022,38(2):472-482.
YU Feng,YU Yang,WANG Deng-hong,et al.Application of Li Isotope in Geothermal Fluid-rock Interaction:A Case Study of Modern Li-rich Geothermal Water in Western Sichuan[J].Acta Petrologica Sinica,2022,38(2):472-482.
[38]吕苑苑.青藏高原盐湖硼、锂同位素变化规律及其对当雄错盐湖资源评价应用[J].地质力学学报,2024,30(1):107-128.
LYU Yuan-yuan.Variation Patterns of Boron and Lithium Isotopes in Salt Lakes on the Qinghai-Tibetan Plateau and Their Application in Evaluating Resources in the Damxung Co Salt Lake[J].Journal of Geomechanics,2024,30(1):107-128.
[39]赵继昌,李文鹏,彭建华,等.唐古拉山发源的河水主要元素与锶同位素来源及环境意义[J].现代地质,2007,21(4):591-599.
ZHAO Ji-chang,LI Wen-peng,PENG Jian-hua,et al.Origin and Environmental Significance of Major Elements and Sr Isotope Ratios in Rivers Originating from Tanggula Mountains[J].Geoscience,2007,21(4):591-599.
[40]董维红,苏小四,谢 渊,等.鄂尔多斯白垩系盆地地下水水-岩反应的锶同位素证据[J].吉林大学学报(地球科学版),2010,40(2):342-348.
DONG Wei-hong,SU Xiao-si,XIE Yuan,et al.Groundwater-rock Interaction in the Ordos Cretaceous Groundwater Basin:Strontium Isotope Evidence[J].Journal of Jilin University(Earth Science Edition),2010,40(2):342-348.
[41]史婷婷,成建梅,解习农,等.松辽盆地北部地层水同位素特征及其地质意义[J].沉积学报,2012,30(2):399-404.
SHI Ting-ting,CHENG Jian-mei,XIE Xi-nong,et al.Isotopic Characteristics of Formation Waters in the North of Songliao Basin and Its Geological Significances[J].Acta Sedimentologica Sinica,2012,30(2):399-404.
[42]苏春利,张 雅,马燕华,等.贵阳市岩溶地下水水化学演化机制:水化学和锶同位素证据[J].地球科学,2019,44(9):2829-2838.
SU Chun-li,ZHANG Ya,MA Yan-hua,et al.Hydrochemical Evolution Processes of Karst Groundwater in Guiyang City:Evidences from Hydrochemistry and 87Sr/86Sr Ratios[J].Earth Science,2019,44(9):2829-2838.
[43]山俊杰,毕有益,邓美洲,等.川西坳陷新场气田须二段气藏地层水成因研究:水化学和锶同位素证据[J].岩石矿物学杂志,2023,42(5):735-744.
SHAN Jun-jie,BI You-yi,DENG Mei-zhou,et al. Hydrochemistry and Sr Isotope Constraints on the Genesis of Formation Water in the 2nd Member of Xujiahe Formation Gas Reservoir in Xinchang Gas Field, Western Sichuan Depression[J].Acta Petrologica et Mineralogica,2023,42(5):735-744.
[44]王 兵,秦西伟,任二峰,等. 柴北缘大柴旦地区地下热水成因:来自水化学及氢、氧、锶同位素的约束[J].矿物岩石地球化学通报,2024,43(1):167-177.
WANG Bing,QIN Xi-wei,REN Er-feng,et al. Gensis of Geothermal Water in the Da Qaidam Area,Northern Margin of the Qaidam Basin:Constraints from Hydrochemistry and Isotopes of Hydrogen-oxygen-strontium[J].Bulletin of Mineralogy,Petrology and Geochemistry,2024,43(1):167-177.
[45]赵 悦,李延河,胡 斌,等.碳酸盐(岩)的锂同位素组成:一种潜在的古海水pH替代性指标[J].地球学报,2020,41(5):613-622.
ZHAO Yue,LI Yan-he,HU Bin,et al.Lithium Isotopic Composition of Marine Carbonate Rocks:A New Proxy for Paleo-pH Reconstruction[J].Acta Geoscientica Sinica,2020,41(5):613-622.
[46]魏帅超,张 薇,付 勇,等. 我国地热水中锂元素分布特征及资源开发利用[J].中国地质,2023,https:∥kns.cnki.net/kcms/detail/11.1167.P.20230505.1132.012.html.
WEI Shuai-chao,ZHANG Wei, FU Yong,et al. Distribution Characteristics and Resource Potential Evalu-ation of Lithium in Geothermal Water in China[J].Geology in China,2023,https:∥kns.cnki.net/kcms/detail/11.1167.P.20230505.1132.012.html.
[47]魏 丽,马尚伟,蒋子文.靖边气田北部马家沟组马五段白云岩、方解石脉地球化学特征及成因[J].中国石油大学学报(自然科学版),2022,46(6):59-69.
WEI Li,MA Shang-wei,JIANG Zi-wen.Geochemical Characteristics and Genesis of Dolomite and Calcite Veins in the Fifth Member of Majiagou Formation in the Northern Jingbian Gas Field[J].Journal of China University of Petroleum(Edition of Natural Science),2022,46(6):59-69.
[48]王利超,胡文瑄,王小林,等.白云岩化过程中锶含量变化及锶同位素分馏特征与意义[J].石油与天然气地质,2016,37(4):464-472.
WANG Li-chao,HU Wen-xuan,WANG Xiao-lin,et al.Variation of Sr Content and 87Sr/86Sr Isotope Fractionation During Dolomitization and Their Implications[J].Oil & Gas Geology,2016,37(4):464-472.
[49]陈郁华.黄海水25 ℃恒温蒸发时的析盐序列及某些微量元素的分布规律[J].地质学报,1983,57(4):379-390.
CHEN Yu-hua.Sequence of Salt Separation and Re-gularity of Some Trace Elements Distribution During Isothermal Evaporation(25 ℃)of the Huanghai Sea Water[J].Acta Geologica Sinica,1983,57(4):379-390.
[50]樊 馥,郑绵平,张永生,等.靖边气田富Br-、I-、Li+、K+油田水的发现及对找钾的启示[J].吉林大学学报(地球科学版),2012,42(增2):141-147.
FAN Fu,ZHENG Mian-ping,ZHANG Yong-sheng,et al.Discovery of Oil Field Water with High Content of Br-,I-,Li+,K+ as the Indication of Finding Potash in Jingbian Gas Field[J].Journal of Jilin Univer-sity(Earth Science Edition),2012,42(S2):141-147.
[51]GODFREY L V,CHAN L H,ALONSO R N,et al.The Role of Climate in the Accumulation of Lithium-rich Brine in the Central Andes[J].Applied Geoche-mistry,2013,38:92-102.

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备注/Memo

备注/Memo:
收稿日期:2024-03-16; 修回日期:2024-05-09
基金项目:中国石油与天然气股份有限公司公关性应用性科技专项项目(2023ZZ31); 中国石油与天然气股份有限公司前瞻性基础性技术攻关项目(2021DJ1504)
*通信作者:李进步(1974-),男,陕西西安人,教授级高级工程师,工学博士,E-mail:ljb2_cq@petrochina.com.cn。
通信作者:王昌勇(1981-),男,四川自贡人,副教授,理学博士,E-mail:wangchangyong09@cdut.cn。
更新日期/Last Update: 2024-10-01