马海盆地深部孔隙卤水矿床水化学特征及成因
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摘要
通过数理统计、聚类以及离子特征系数等分析方法,对柴达木马海盆地的深部砂砾石层孔隙卤水水化学特征进行了分析。卤水离子浓度空间分布特征表现为pH、Cl~-、TDS和Na~+浓度值变化范围较小,分布均匀,而K~+、Rb~+以及Br~-、Mg~(2+)、Li~+、Sr~(2+)、I~-、B_2O_3、Ca~(2+)、Cs~+、NO■、SO■等离子浓度分布不均匀,差异显著;Cl~-、TDS、Na~+、K~+、Mg~(2+)和Li~+与SO■聚为一个亚类,表明卤水演化过程中有酸性液体的参与;K~+含量自西向东有增大的趋势,与Mg~(2+)和Li~+的变化具有相关性;离子特征系数反映出蒸发残余及盐岩溶解的多源性特征。研究区水化学类型为单一的氯化钠型,这种单一的物源可能与推测的更新统下伏盐岩层有关。
Analysis of the hydrochemical characteristics and origin of deep sandy gravel brine in Mahai Basin is based on mathematical statistics, cluster analysis, and ion characteristic coefficients. The spatial distribution characteristics of brine ion concentrations shows that the ion concentrations of pH, Cl~-, TDS, and Na~+ have a narrow range of change and uniform distribution, while the ion concentrations of K~+, Rb~+, Br~-, Mg~(2+), Li~+, Sr~(2+), I~-, B_2O_3, Ca~(2+), Cs~+, NO~-_3, and SO■ exhibit significant variation and uneven distribution. Cluster analysis indicates that Cl~-, TDS, Na~+, K~+, Mg~(2+), Li~+, and SO■ piled, which shows the evolution of brine is related to the joining of acid liquid. K~+, which has correlation with Mg~(2+) and Li~+, shows an increasing trend from west to east in the variety graph of ion contents. The characteristic coefficients and higher contents of trace ions suggest that the brine has multifocal features of evaporation residue and gypsum dissolution. The Na~+, K~+, and Mg~(2+)//Cl~--H_2O four-element system mesostationary phase, as well as the analysis of ionic characteristic coefficients in brine, indicate that the hydrochemical type is the single chloride-type, which reflects the single provenance and may have a relationship with the stochastic underlying salt strata of the Pleistocene.
Analysis of the hydrochemical characteristics and origin of deep sandy gravel brine in Mahai Basin is based on mathematical statistics, cluster analysis, and ion characteristic coefficients. The spatial distribution characteristics of brine ion concentrations shows that the ion concentrations of pH, Cl~-, TDS, and Na~+ have a narrow range of change and uniform distribution, while the ion concentrations of K~+, Rb~+, Br~-, Mg~(2+), Li~+, Sr~(2+), I~-, B_2O_3, Ca~(2+), Cs~+, NO~-_3, and SO■ exhibit significant variation and uneven distribution. Cluster analysis indicates that Cl~-, TDS, Na~+, K~+, Mg~(2+), Li~+, and SO■ piled, which shows the evolution of brine is related to the joining of acid liquid. K~+, which has correlation with Mg~(2+) and Li~+, shows an increasing trend from west to east in the variety graph of ion contents. The characteristic coefficients and higher contents of trace ions suggest that the brine has multifocal features of evaporation residue and gypsum dissolution. The Na~+, K~+, and Mg~(2+)//Cl~--H_2O four-element system mesostationary phase, as well as the analysis of ionic characteristic coefficients in brine, indicate that the hydrochemical type is the single chloride-type, which reflects the single provenance and may have a relationship with the stochastic underlying salt strata of the Pleistocene.
引文
[1] 郑绵平,张雪飞,侯献华,等.青藏高原晚新生代湖泊地质环境与成盐成藏作用[J].地球学报,2013,34(2):129-138.[Zheng Mianping,Zhang Xuefei,Hou Xianhua,et al.Geological environments of the Late Cenozoic lakes and salt-forming and oil-gas pool-forming actions in the Tibetan Plateau[J].Acta Geoscientica Sinica,2013,34(2):129-138.]
[2] 郑绵平.论中国盐湖[J].矿床地质,2001,20(2):181-189.[Zheng Mianping.On saline lakes of China[J].Mineral Deposits,2001,20(2):181-189.]
[3] 郑喜玉,刘建华.新疆盐湖卤水成分及其成因[J].地理科学,1996,16(2):115-123.[Zheng Xiyu,Liu Jianhua.The composition and origin of salt lake brines in Xinjiang[J].Scientia Geographica Sinica,1996,16(2):115-123.]
[4] 刘卫国,肖应凯,孙大鹏,等.马海盐湖区卤水和盐类矿物的氯同位素特征及意义[J].盐湖研究,1995,3(2):29-33.[Liu Weiguo,Xiao Yingkai,Sun Dapeng,et al.Characteristics and significance of chlorine isotope of brine and deposits in the Mahai Salt Lakes[J].Journal of Salt Lake Research,1995,3(2):29-33.]
[5] 雷延智,潘玉麟.巴仑马海盐湖低品位卤水自然蒸发试验研究[J].化工矿物与加工,2006(6):11-14.[Lei Yanzhi,Pan Yulin.Natural evaporation of low grade brine in Balunmahai Salt Lake[J].Industrial Minerals & Processing,2006(6):11-14.]
[6] 郭爱武,李刚.马海盐湖卤水自然蒸发实验研究[J].盐湖研究,2008,16(3):30-32.[Guo Aiwu,Li Gang.Study on natural evaporation of brine in Mahai Salt Lakes[J].Journal of Salt Lake Research,2008,16(3):30-32.]
[7] 潘晓晨,成怀刚,程芳琴.马海盐湖溶采卤水高温梯级蒸发实验研究[J].无机盐工业,2013,45(6):15-18.[Pan Xiaochen,Cheng Huaigang,Cheng Fangqin.Study on stepped high temperatrue evaporation of dissolved brine in Mahai Salt Lakes[J].Inorganic Chemicals Industry,2013,45(6):15-18.]
[8] 汤玉兰.青海马海盐湖富钾卤水地球化学特征及其成因研究[D].北京:中国地质大学(北京),2015.[Tang Yulan.Study on geochemical characteristics and genesis of potassium-rich brine in Mahai Salt Lake in Qinghai province[D].Beijing:China University of Geosciences,2015.]
[9] 马金元,胡生忠,田向东.柴达木盆地马海钾盐矿床沉积环境与开发[J].盐湖研究,2010,18(3):9-17.[Ma Jinyuan,Hu Shengzhong,Tian Xiangdong.Sedimentary environment and exploitation of Maihai potash deposits in Qaidam Basin[J].Journal of Salt Lake Research,2010,18(3):9-17.]
[10] 焦鹏程,张建伟,姚佛军,等.马海盐湖深部卤水钾盐勘查与研究进展[J].矿床地质,2016,35(6):1305-1308.[Jiao Pengcheng,Zhang Jianwei,Yao Fojun,et al.Potassium exploration and research progress of deep brine in Mahai Salt Lake[J].Mineral Deposits,2016,35(6):1305-1308.]
[11] 王宇涵.青海柴达木盆地马海盐湖第四纪沉积环境研究[D].北京:中国地质大学(北京),2016.[Wang Yuhan.Research on sedimentary environment of mohair salt lake in Quaternary in the Qaidam Basin Qinghai province[D].Beijing:China University of Geosciences,2016.]
[12] 李洪普,郑绵平.柴达木盆地西部深层卤水钾盐矿成矿地质特征[J].矿床地质,2014,39(S1):935-936.[Li Hongpu,Zheng Mianping.Mineralization geological characteristics of deep brine potassium mine in the west of Qaidam Basin[J].Mineral Deposits,2014,39(S1):935-936.]
[13] 李洪普,郑绵平,侯献华,等.柴达木黑北凹地早更新世新型砂砾层卤水水化学特征与成因[J].地球科学——中国地质大学学报,2014,39(10):1333-1342.[Li Hongpu,Zheng Mianping,Hou Xianhua,et al.Hydrochemistry characteristics and origin of new brine sandy gravel in Early Pleistocene of Heibei Concave in Qaidam Basin[J].Earth Science—Journal of China University of Geosciences,2014,39(10):1333-1342.]
[14] 李洪普,郑绵平,侯献华,等.柴达木西部南翼山构造富钾深层卤水矿的控制因素及水化学特征[J].地球学报,2015,36(1):41-50.[Li Hongpu,Zheng Mianping,Hou Xianhua,et al.Control factors and water chemical characteristics of potassium-rich deep brine in nanyishan structure of western Qaidam Basin[J].Acta Geoscientica Sinica,2015,36(1):41-50.]
[15] 田向东,李洪普,王云生,等.柴达木北部新盐带卤水水化学特征研究[J].盐业与化工,2013,42(12):8-12.[Tian Xiangdong,Li Hongpu,Wang Yunsheng,et al.Study on the hydrochemical characteristics of the Xinyandai latent brine in the north of Qaidam Basin[J].Journal of Salt and Chemical Industry,2013,42(12):8-12.]
[16] 郑绵平,刘喜方.青藏高原盐湖水化学及其矿物组合特征[J].地质学报,2010,84(11):1585-1600.[Zheng Mianping,Liu Xifang.Hydrochemistry and minerals assemblages of salt lakes in the Qinghai-Tibet Plateau,China[J].Acta Geologica Sinica,2010,84(11):1585-1600.]
[17] 张西营,马海洲,高东林,等.柴达木盆地西台吉乃尔盐湖矿区卤水水化学特征[J].盐湖研究,2007,15(2):12-20.[Zhang Xiying,Ma Haizhou,Gao Donglin,et al.Hydrochemical characteristics of brines in the mining area of West Taijinar Salt Lake in Qaidam Basin[J].Journal of Salt Lake Research,2007,15(2):12-20.]
[18] 叶传永,王志明,赵世勤,等.青海省尕斯库勒盐湖卤水水化学特征初步研究[J].盐湖研究,2013,21(1):14-23,37.[Ye Chuanyong,Wang Zhiming,Zhao Shiqin,et al.Priliminary study of the hydrochemical characteristics of brines in the Gas Hure Salt Lake,Qinghai province[J].Journal of Salt Lake Research,2013,21(1):14-23,37.]
[19] 樊启顺,马海洲,谭红兵,等.柴达木盆地西部典型地区油田卤水水化学异常及资源评价[J].盐湖研究,2007,15(4):6-12.[Fan Qishun,Ma Haizhou,Tan Hongbing,et al.Hydrochemical anomaly and resources evaluation of the oil field brines in the typical area of western Qaidam Basin[J].Journal of Salt Lake Research,2007,15(4):6-12.]
[20] 樊启顺,马海州,谭红兵,等.柴达木盆地西部卤水特征及成因探讨[J].地球化学,2007,36(6):601-611.[Fan Qishun,Ma Haizhou,Tan Hongbing,et al.Characteristics and origin of brines in western Qaidam Basin[J].Geochimica,2007,36(6):601-611.]
[21] 单慧媚,马腾,刘存富,等.有机溴化物的溴同位素测试技术及其生物地球化学指示意义[J].地球科学进展,2011,26(8):811-821.[Shan Huimei,Ma Teng,Liu Fucun,et al.An overview of analytical methods of bromine stable isotope (81Br) of BOCs and its significance to biogeochemical cycle[J].Advances in Earth Science,2011,26(8):811-821.]
[22] 曾昭华,曾雪萍.地下水中溴的形成及其与人群健康的关系[J].吉林地质,2001,20(1):57-59.[Zeng Zhaohua,Zeng Xueping.The formation of trace element of Br in groundwater and its relationship with the health of People’s community[J].Jilin Geology,2001,20(1):57-59.]
[23] 李廷伟,李建森,马海洲,等.柴达木盆地西部油田卤水硼同位素地球化学研究[J].盐湖研究,2013,21(2):1-9.[Li Tingwei,Li Jiansen,Ma Haizhou,et al.Boron isotope geochemical study on oil-field brine in western Qaidam Basin[J].Journal of Salt Lake Research,2013,21(2):1-9.]
[24] 肖荣阁,大井隆夫,蔡克勤,等.硼及硼同位素地球化学在地质研究中的应用[J].地学前缘,1999,6(2):361-367.[Xiao Rongge,Takao Oi,Cai Keqin,et al.Application of boron and boron isotopic geochemistry in the study of geological process[J].Earth Science Frontiers,1999,6(2):361-367.]
[25] 马万栋.塔里木盆地西部岩盐的地球化学特征及钾盐远景区预测研究[D].西宁:中国科学院研究生院(青海盐湖研究所),2004.[Ma Wandong.The research on geochemical characteristics and potass forecast of halite in western Tarim Basin[D].Xining:Graduate School of Chinese Academy of Sciences (Qinghai Salt Lake Institute),2004.]
[26] 刘勇平,周敬,韩凤清,等.青海可可西里东部盐湖水化学及沉积特征初步研究[J].盐湖研究,2009,17(3):10-16.[Liu Yongping,Zhou Jing,Han Fengqing,et al.Preliminary study of hydrochemistry and sedimentary characteristics of salt lakes in eastern Hoh Xil region[J].Journal of Salt Lake Research,2009,17(3):10-16.]
[27] 张西营,马海洲,谭红兵.Sr的地球化学指示意义及其应用[J].盐湖研究,2002,10(3):38-44.[Zhang Xiying,Ma Haizhou,Tan Hongbing.The indicative significance and application of strontium in geochemistry[J].Journal of Salt Lake Research,2002,10(3):38-44.]
[28] 樊启顺,马海洲,谭红兵,等.柴达木盆地西部卤水水化学特征与找钾研究[J].地球学报,2007,28(5):446-455.[Fan Qishun,Ma Haizhou,Tan Hongbing,et al.Hydrochemical characteristics of brines and potassium-prospecting researches in western Qaidam Basin[J].Acta Geoscientica Sinica,2007,28(5):446-455.]
[29] 李廷伟,谭红兵,樊启顺.柴达木盆地西部地下卤水水化学特征及成因分析[J].盐湖研究,2006,14(4):26-32.[Li Tingwei,Tan Hongbing,Fan Qishun.Hydrochemical characteristics and origin analysis of the underground brines in west Qaidam Basin[J].Journal of Salt Lake Research,2006,14(4):26-32.]
[30] 韩佳君,周训,姜长龙,等.柴达木盆地西部地下卤水水化学特征及其起源演化[J].现代地质,2013,27(6):1454-1464.[Han Jiajun,Zhou Xun,Jiang Changlong,et al.Hydrochemical characteristics,origin and evolution of the subsurface brines in western Qaidam Basin[J].Geoscience,2013,27(6):1454-1464.]
[31] 谭红兵,曹成东,李廷伟,等.柴达木盆地西部古近系和新近系油田卤水资源水化学特征及化学演化[J].古地理学报,2007,9(3):313-320.[Tan Hongbing,Cao Chengdong,Li Tingwei,et al.Hydrochemistry characteristics and chemical evolution of oilfield brines of the Paleogene and Neogene in western Qaidam Basin[J].Journal of Palaeogeography,2007,9(3):313-320.]
[32] 周训,曹琴,尹菲,等.四川盆地东部高褶带三叠系地层卤水和温泉的地球化学特征及成因[J].地质学报,2015,89(11):1908-1920.[Zhou Xun,Cao Qin,Yin Fei,et al.Characteristics of the brines and hot springs in the Triassic carbonates in the high and steep fold zone of the eastern Sichuan Basin[J].Acta Geologica Sinica,2015,89(11):1908-1920.]
[33] 周训.四川盆地龙女寺储卤构造深层地下卤水的水文地球化学特征及成因[J].现代地质,1993,7(1):83-92.[Zhou Xun.Hydrogeochemical characteristics and formation of subsurface brines of deep aquifers in Longnu temple brine-bearing structure,Sichuan Basin[J].Geoscience,1993,7(1):83-92.]
[2] 郑绵平.论中国盐湖[J].矿床地质,2001,20(2):181-189.[Zheng Mianping.On saline lakes of China[J].Mineral Deposits,2001,20(2):181-189.]
[3] 郑喜玉,刘建华.新疆盐湖卤水成分及其成因[J].地理科学,1996,16(2):115-123.[Zheng Xiyu,Liu Jianhua.The composition and origin of salt lake brines in Xinjiang[J].Scientia Geographica Sinica,1996,16(2):115-123.]
[4] 刘卫国,肖应凯,孙大鹏,等.马海盐湖区卤水和盐类矿物的氯同位素特征及意义[J].盐湖研究,1995,3(2):29-33.[Liu Weiguo,Xiao Yingkai,Sun Dapeng,et al.Characteristics and significance of chlorine isotope of brine and deposits in the Mahai Salt Lakes[J].Journal of Salt Lake Research,1995,3(2):29-33.]
[5] 雷延智,潘玉麟.巴仑马海盐湖低品位卤水自然蒸发试验研究[J].化工矿物与加工,2006(6):11-14.[Lei Yanzhi,Pan Yulin.Natural evaporation of low grade brine in Balunmahai Salt Lake[J].Industrial Minerals & Processing,2006(6):11-14.]
[6] 郭爱武,李刚.马海盐湖卤水自然蒸发实验研究[J].盐湖研究,2008,16(3):30-32.[Guo Aiwu,Li Gang.Study on natural evaporation of brine in Mahai Salt Lakes[J].Journal of Salt Lake Research,2008,16(3):30-32.]
[7] 潘晓晨,成怀刚,程芳琴.马海盐湖溶采卤水高温梯级蒸发实验研究[J].无机盐工业,2013,45(6):15-18.[Pan Xiaochen,Cheng Huaigang,Cheng Fangqin.Study on stepped high temperatrue evaporation of dissolved brine in Mahai Salt Lakes[J].Inorganic Chemicals Industry,2013,45(6):15-18.]
[8] 汤玉兰.青海马海盐湖富钾卤水地球化学特征及其成因研究[D].北京:中国地质大学(北京),2015.[Tang Yulan.Study on geochemical characteristics and genesis of potassium-rich brine in Mahai Salt Lake in Qinghai province[D].Beijing:China University of Geosciences,2015.]
[9] 马金元,胡生忠,田向东.柴达木盆地马海钾盐矿床沉积环境与开发[J].盐湖研究,2010,18(3):9-17.[Ma Jinyuan,Hu Shengzhong,Tian Xiangdong.Sedimentary environment and exploitation of Maihai potash deposits in Qaidam Basin[J].Journal of Salt Lake Research,2010,18(3):9-17.]
[10] 焦鹏程,张建伟,姚佛军,等.马海盐湖深部卤水钾盐勘查与研究进展[J].矿床地质,2016,35(6):1305-1308.[Jiao Pengcheng,Zhang Jianwei,Yao Fojun,et al.Potassium exploration and research progress of deep brine in Mahai Salt Lake[J].Mineral Deposits,2016,35(6):1305-1308.]
[11] 王宇涵.青海柴达木盆地马海盐湖第四纪沉积环境研究[D].北京:中国地质大学(北京),2016.[Wang Yuhan.Research on sedimentary environment of mohair salt lake in Quaternary in the Qaidam Basin Qinghai province[D].Beijing:China University of Geosciences,2016.]
[12] 李洪普,郑绵平.柴达木盆地西部深层卤水钾盐矿成矿地质特征[J].矿床地质,2014,39(S1):935-936.[Li Hongpu,Zheng Mianping.Mineralization geological characteristics of deep brine potassium mine in the west of Qaidam Basin[J].Mineral Deposits,2014,39(S1):935-936.]
[13] 李洪普,郑绵平,侯献华,等.柴达木黑北凹地早更新世新型砂砾层卤水水化学特征与成因[J].地球科学——中国地质大学学报,2014,39(10):1333-1342.[Li Hongpu,Zheng Mianping,Hou Xianhua,et al.Hydrochemistry characteristics and origin of new brine sandy gravel in Early Pleistocene of Heibei Concave in Qaidam Basin[J].Earth Science—Journal of China University of Geosciences,2014,39(10):1333-1342.]
[14] 李洪普,郑绵平,侯献华,等.柴达木西部南翼山构造富钾深层卤水矿的控制因素及水化学特征[J].地球学报,2015,36(1):41-50.[Li Hongpu,Zheng Mianping,Hou Xianhua,et al.Control factors and water chemical characteristics of potassium-rich deep brine in nanyishan structure of western Qaidam Basin[J].Acta Geoscientica Sinica,2015,36(1):41-50.]
[15] 田向东,李洪普,王云生,等.柴达木北部新盐带卤水水化学特征研究[J].盐业与化工,2013,42(12):8-12.[Tian Xiangdong,Li Hongpu,Wang Yunsheng,et al.Study on the hydrochemical characteristics of the Xinyandai latent brine in the north of Qaidam Basin[J].Journal of Salt and Chemical Industry,2013,42(12):8-12.]
[16] 郑绵平,刘喜方.青藏高原盐湖水化学及其矿物组合特征[J].地质学报,2010,84(11):1585-1600.[Zheng Mianping,Liu Xifang.Hydrochemistry and minerals assemblages of salt lakes in the Qinghai-Tibet Plateau,China[J].Acta Geologica Sinica,2010,84(11):1585-1600.]
[17] 张西营,马海洲,高东林,等.柴达木盆地西台吉乃尔盐湖矿区卤水水化学特征[J].盐湖研究,2007,15(2):12-20.[Zhang Xiying,Ma Haizhou,Gao Donglin,et al.Hydrochemical characteristics of brines in the mining area of West Taijinar Salt Lake in Qaidam Basin[J].Journal of Salt Lake Research,2007,15(2):12-20.]
[18] 叶传永,王志明,赵世勤,等.青海省尕斯库勒盐湖卤水水化学特征初步研究[J].盐湖研究,2013,21(1):14-23,37.[Ye Chuanyong,Wang Zhiming,Zhao Shiqin,et al.Priliminary study of the hydrochemical characteristics of brines in the Gas Hure Salt Lake,Qinghai province[J].Journal of Salt Lake Research,2013,21(1):14-23,37.]
[19] 樊启顺,马海洲,谭红兵,等.柴达木盆地西部典型地区油田卤水水化学异常及资源评价[J].盐湖研究,2007,15(4):6-12.[Fan Qishun,Ma Haizhou,Tan Hongbing,et al.Hydrochemical anomaly and resources evaluation of the oil field brines in the typical area of western Qaidam Basin[J].Journal of Salt Lake Research,2007,15(4):6-12.]
[20] 樊启顺,马海州,谭红兵,等.柴达木盆地西部卤水特征及成因探讨[J].地球化学,2007,36(6):601-611.[Fan Qishun,Ma Haizhou,Tan Hongbing,et al.Characteristics and origin of brines in western Qaidam Basin[J].Geochimica,2007,36(6):601-611.]
[21] 单慧媚,马腾,刘存富,等.有机溴化物的溴同位素测试技术及其生物地球化学指示意义[J].地球科学进展,2011,26(8):811-821.[Shan Huimei,Ma Teng,Liu Fucun,et al.An overview of analytical methods of bromine stable isotope (81Br) of BOCs and its significance to biogeochemical cycle[J].Advances in Earth Science,2011,26(8):811-821.]
[22] 曾昭华,曾雪萍.地下水中溴的形成及其与人群健康的关系[J].吉林地质,2001,20(1):57-59.[Zeng Zhaohua,Zeng Xueping.The formation of trace element of Br in groundwater and its relationship with the health of People’s community[J].Jilin Geology,2001,20(1):57-59.]
[23] 李廷伟,李建森,马海洲,等.柴达木盆地西部油田卤水硼同位素地球化学研究[J].盐湖研究,2013,21(2):1-9.[Li Tingwei,Li Jiansen,Ma Haizhou,et al.Boron isotope geochemical study on oil-field brine in western Qaidam Basin[J].Journal of Salt Lake Research,2013,21(2):1-9.]
[24] 肖荣阁,大井隆夫,蔡克勤,等.硼及硼同位素地球化学在地质研究中的应用[J].地学前缘,1999,6(2):361-367.[Xiao Rongge,Takao Oi,Cai Keqin,et al.Application of boron and boron isotopic geochemistry in the study of geological process[J].Earth Science Frontiers,1999,6(2):361-367.]
[25] 马万栋.塔里木盆地西部岩盐的地球化学特征及钾盐远景区预测研究[D].西宁:中国科学院研究生院(青海盐湖研究所),2004.[Ma Wandong.The research on geochemical characteristics and potass forecast of halite in western Tarim Basin[D].Xining:Graduate School of Chinese Academy of Sciences (Qinghai Salt Lake Institute),2004.]
[26] 刘勇平,周敬,韩凤清,等.青海可可西里东部盐湖水化学及沉积特征初步研究[J].盐湖研究,2009,17(3):10-16.[Liu Yongping,Zhou Jing,Han Fengqing,et al.Preliminary study of hydrochemistry and sedimentary characteristics of salt lakes in eastern Hoh Xil region[J].Journal of Salt Lake Research,2009,17(3):10-16.]
[27] 张西营,马海洲,谭红兵.Sr的地球化学指示意义及其应用[J].盐湖研究,2002,10(3):38-44.[Zhang Xiying,Ma Haizhou,Tan Hongbing.The indicative significance and application of strontium in geochemistry[J].Journal of Salt Lake Research,2002,10(3):38-44.]
[28] 樊启顺,马海洲,谭红兵,等.柴达木盆地西部卤水水化学特征与找钾研究[J].地球学报,2007,28(5):446-455.[Fan Qishun,Ma Haizhou,Tan Hongbing,et al.Hydrochemical characteristics of brines and potassium-prospecting researches in western Qaidam Basin[J].Acta Geoscientica Sinica,2007,28(5):446-455.]
[29] 李廷伟,谭红兵,樊启顺.柴达木盆地西部地下卤水水化学特征及成因分析[J].盐湖研究,2006,14(4):26-32.[Li Tingwei,Tan Hongbing,Fan Qishun.Hydrochemical characteristics and origin analysis of the underground brines in west Qaidam Basin[J].Journal of Salt Lake Research,2006,14(4):26-32.]
[30] 韩佳君,周训,姜长龙,等.柴达木盆地西部地下卤水水化学特征及其起源演化[J].现代地质,2013,27(6):1454-1464.[Han Jiajun,Zhou Xun,Jiang Changlong,et al.Hydrochemical characteristics,origin and evolution of the subsurface brines in western Qaidam Basin[J].Geoscience,2013,27(6):1454-1464.]
[31] 谭红兵,曹成东,李廷伟,等.柴达木盆地西部古近系和新近系油田卤水资源水化学特征及化学演化[J].古地理学报,2007,9(3):313-320.[Tan Hongbing,Cao Chengdong,Li Tingwei,et al.Hydrochemistry characteristics and chemical evolution of oilfield brines of the Paleogene and Neogene in western Qaidam Basin[J].Journal of Palaeogeography,2007,9(3):313-320.]
[32] 周训,曹琴,尹菲,等.四川盆地东部高褶带三叠系地层卤水和温泉的地球化学特征及成因[J].地质学报,2015,89(11):1908-1920.[Zhou Xun,Cao Qin,Yin Fei,et al.Characteristics of the brines and hot springs in the Triassic carbonates in the high and steep fold zone of the eastern Sichuan Basin[J].Acta Geologica Sinica,2015,89(11):1908-1920.]
[33] 周训.四川盆地龙女寺储卤构造深层地下卤水的水文地球化学特征及成因[J].现代地质,1993,7(1):83-92.[Zhou Xun.Hydrogeochemical characteristics and formation of subsurface brines of deep aquifers in Longnu temple brine-bearing structure,Sichuan Basin[J].Geoscience,1993,7(1):83-92.]
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