Chengdu Center, China Geological SurveyHost
Advanced Search
Previous Article Next Article
2023 Vol. 43, No. 2
Article Contents
Article navigation > Sedimentary Geology and Tethyan Geology > 2023 > 43(2): 311-321
Next Article Previous Article

SHI Hongjie, LIU Mingliang, WEI Xing, CAO Yuanyuan, SHANG Jianbo. 2023. Geochemical characteristics and formation mechanisms of the geothermal waters from the Mapamyumco, Tibet. Sedimentary Geology and Tethyan Geology, 43(2): 311-321. doi: 10.19826/j.cnki.1009-3850.2023.04009
Citation: SHI Hongjie, LIU Mingliang, WEI Xing, CAO Yuanyuan, SHANG Jianbo. 2023. Geochemical characteristics and formation mechanisms of the geothermal waters from the Mapamyumco, Tibet. Sedimentary Geology and Tethyan Geology, 43(2): 311-321. doi: 10.19826/j.cnki.1009-3850.2023.04009
shu

Geochemical characteristics and formation mechanisms of the geothermal waters from the Mapamyumco, Tibet

  • 1.

    Hubei Key Laboratory of Petroleum Geochemistry and Environment & College of Resources and Environment, Yangtze University, Wuhan 430100, China

  • 2.

    Geophysical and Geochemical Exploration Institute of Ningxia Hui Autonomous Region, Yinchuan 750001, China

More Information
Received Date:  07 January 2023
Revised Date:  11 April 2023
Accepted Date:  11 April 2023
Publish Date:  30 June 2023
    Abstract

  • Tibet is located at the Indian-Eurasia collision orogenic belt, where the tectonic activity is intense, resulting in abundant geothermal resources. In this study, the hot spring samples from the Mapamyumco geothermal field situated at the Ngari Prefecture of Tibet with strong geothermal activity were collected for hydrochemical analysis. Based on the hydrochemical characteristics of the geothermal water, the equilibrium state and temperature of the reservoir was evaluated; the hydrogeochemical processes of deep geothermal fluid was analyzed; and the heat source type of the geothermal system was identified. These results are contributed to clarify its genesis mechanism. This study shows that: the geothermal water in the area are mainly alkaline Cl-Na type or HCO3-Cl-Na type and acidic SO4-Na type water; the geothermal water has reached a complete equilibrium state with the thermal reservoir rocks at depth, and the thermal reservoir temperature is about 200℃ based on geochemical geothermometer calculation; surface geothermal manifestations, hydrochemical characteristics of geothermal water, and the reservoir temperatures reveal that Mapamyumco geothermal field is a magmatic geothermal system, and different types of geothermal water are formed by different hydrogeochemical processes during the upward transport of deep parent geothermal fluid along the fault.

    • FullText(HTML)
  • 加载中
    • References
  • [1] Arnórsson S and Andrésdóttir A, 1995. Processes controlling the distribution of boron and chlorine in natural waters in Iceland[J]. Geochimica et Cosmochimica Acta, 59（20）: 4125-4146. doi: 10.1016/0016-7037(95)00278-8

    CrossRef Google Scholar

    [2] Fournier R O, 1977. Chemical geothermometers and mixing models for geothermal systems[J]. Geothermics, 5（1-4）: 41-50. doi: 10.1016/0375-6505(77)90007-4

    CrossRef Google Scholar

    [3] 高洪雷, 胡志华, 万汉平, 等, 2023. 西藏谷露地热田地热地质特征[J]. 地球科学, 48（3）: 1014-1029

    Google Scholar

    Gao H L, Hu Z H, Wan H P, et al. , 2023. Characteristics of geothermal geology of the Gulu geothermal field in Tibet[J]. Earth Science, 48（3）: 1014-1029.

    Google Scholar

    [4] Giggenbach W F, Garcia P N, Londoño C A, et al. , 1990. The chemistry of fumarolic vapor and thermal-spring discharges from the Nevado del Ruiz volcanic-magmatic-hydrothermal system, Colombia[J]. Journal of Volcanology and Geothermal Research, 42（1-2）: 13-39. doi: 10.1016/0377-0273(90)90067-P

    CrossRef Google Scholar

    [5] Giggenbach W F, Sheppard D S, Robinson B W, et al. , 1994. Geochemical structure and position of the Waiotapu geothermal field, New Zealand[J]. Geothermics, 23（5）: 599-644.

    Google Scholar

    [6] Giggenbach W F, 1988. Geothermal solute equilibria. Derivation of Na-K-Mg-Ca geoindicators[J]. Geochimica et Cosmochimica Acta, 52（12）: 2749-2765. doi: 10.1016/0016-7037(88)90143-3

    CrossRef Google Scholar

    [7] Guo Q H, Liu M L, Li J X, et al. , 2017. Fluid geochemical constraints on the heat source and reservoir temperature of the Banglazhang hydrothermal system, Yunnan-Tibet Geothermal Province, China[J]. Journal of Geochemical Exploration, 172: 109-119. doi: 10.1016/j.gexplo.2016.10.012

    CrossRef Google Scholar

    [8] Guo Q H, Liu M L, Li J X, et al. , 2014. Acid hot springs discharged from the Rehai hydrothermal system of the Tengchong volcanic area （China）: formed via magmatic fluid absorption or geothermal steam heating?[J]. Bulletin of Volcanology, 76（10）: 1 − 12（Article 868）.

    Google Scholar

    [9] Guo Q H, Liu M L, Luo L, et al. , 2019. Geochemical controls on magnesium and its speciation in various types of geothermal waters from typical felsic-rock-hosted hydrothermal systems in China[J]. Geothermics, 81: 185-197. doi: 10.1016/j.geothermics.2019.05.006

    CrossRef Google Scholar

    [10] Guo Q H, Wang Y X and Liu W, 2008. B, As, and F contamination of river water due to wastewater discharge of the Yangbajing geothermal power plant, Tibet, China[J]. Environmental Geology, 56（1）: 197-205. doi: 10.1007/s00254-007-1155-2

    CrossRef Google Scholar

    [11] 郭清海, 2020. 岩浆热源型地热系统及其水文地球化学判据[J]. 地质学报, 94（12）: 3544-3554

    Google Scholar

    Guo Q H, 2020. Magma-heated geothermal systems and hydrogeochemical evidence of their occurrence[J]. Acta Geologica Sinica, 94（12）: 3544-3554.

    Google Scholar

    [12] 河北省地质调查院区调所, 2005.1∶25万亚热幅、普兰县幅、霍尔巴幅、巴巴扎东幅（国内部分）地质调查成果与进展[J]. 沉积与特提斯地质, Z1: 80-86 doi: 10.3969/j.issn.1009-3850.2005.03.013

    CrossRef Google Scholar

    Hebei Institute of Geological Survey, 2005.1: 250 000 Yagra, Burang, Horba and Babazhadong Sheets in Xizang[J]. Sedimentary Geology and Tethyan Geology, Z1: 80-86. doi: 10.3969/j.issn.1009-3850.2005.03.013

    CrossRef Google Scholar

    [13] 胡先才, 索加, 多吉, 2002. 西藏高温地热资源特征及开发远景分析[J]. 西藏地质, 2: 80-85

    Google Scholar

    Hu X C, SUO J, Duo J, 2002. Characteristics and development prospects of high temperature geothermal resources in Tibet[J]. Geology of Tibet, 2: 80-85.

    Google Scholar

    [14] Li J X, Wu Z H, Tian G H, et al. , 2022. Processes controlling the hydrochemical composition of geothermal fluids in the sandstone and dolostone reservoirs beneath the sedimentary basin in north China[J]. Applied Geochemistry, 138: 105211. doi: 10.1016/j.apgeochem.2022.105211

    CrossRef Google Scholar

    [15] 李文, 孔祥军, 袁利娟, 等, 2020. 中国地热资源概况及开发利用建议[J]. 中国矿业, 29（S1）: 22-26

    Google Scholar

    Li W, Kong X J, Yuan L J, et al. , 2020. General situation and suggestions of development and utilization of geothermal resources in China[J]. China Mining Magazine, 29（S1）: 22-26.

    Google Scholar

    [16] 李振清, 2002. 青藏高原碰撞造山过程中的现代热水活动[D]. 北京: 中国地质科学院.

    Google Scholar

    Li Z Q, 2002. Present hydrothermal activities during collisional orogenics of the Tibetan Plateau[D]. Beijing: Chinese Academy of Geological Sciences.

    Google Scholar

    [17] 廖志杰, 赵平, 1999. 滇藏地热带: 地热资源和典型地热系统[M]. 北京: 科学出版社.

    Google Scholar

    Liao Z J, Zhao P, 1999. Yunnan−Tibet Geothermal Belt−Geothermal resources and case histories[M]. Science Press, Beijing.

    Google Scholar

    [18] Liu M L, Guo Q H, Geng W, et al. , 2019. Boron geochemistry of the geothermal waters from two typical hydrothermal systems in Southern Tibet （China）: Daggyai and Quzhuomu[J]. Geothermics, 82: 190-202. doi: 10.1016/j.geothermics.2019.06.009

    CrossRef Google Scholar

    [19] 吕苑苑, 赵平, 许荣华, 等, 2012. 西藏羊八井地热田硼同位素地球化学特征初步研究[J]. 地质科学, 47（1）: 251-264

    Google Scholar

    Lv Y Y, Zhao P, Xu R H, et al. , 2012. Geochemical study on boron isotopes in the Yangbajing geothermal field, Tibet[J]. Chinese Journal of Geology, 47（1）: 251-264.

    Google Scholar

    [20] 庞忠和, 汪集旸, 樊志成, 1990. 利用SiO2混合模型计算漳州地热田热储温度[J]. 科学通报, 1: 57-59

    Google Scholar

    Pang Z H, Wang J Y, Fan Z C, 1990. Using the SiO2 mixing model to calculate Zhang-zhou geothermal heat storage temperature[J]. Chinese Science Bulletin, 1: 57-59.

    Google Scholar

    [21] 沈立成, 伍坤宇, 肖琼, 等, 2011. 西藏地热异常区CO2脱气研究: 以朗久和搭格架地热区为例[J]. 科学通报, 56（26）: 2198-2208 doi: 10.1360/csb2011-56-26-2198

    CrossRef Google Scholar

    Shen L C, Wu K Y, Xiao Q, et al. , 2011. Carbon dioxide degassing flux from two geothermal fields in Tibet, China[J]. Chinese Science Bulletin, 56（26）: 2198-2208. doi: 10.1360/csb2011-56-26-2198

    CrossRef Google Scholar

    [22] 佟伟, 廖志杰, 刘时彬, 等, 2000. 西藏温泉志[M]. 北京: 科学出版社.

    Google Scholar

    Tong W, Liao Z J, Liu S B, et al. , 2000. Tibetan Hot Springs[M]. Science Press, Beijing.

    Google Scholar

    [23] 佟伟, 章铭陶, 张知非, 等, 1981. 西藏地热[M]. 北京: 科学出版社.

    Google Scholar

    Tong W, Zhang M T, Zhang Z F, et al. , 1981. Geothermal Heat in Tibet[M]. Science Press, Beijing.

    Google Scholar

    [24] Wang C G and Zheng M P, 2019. Hydrochemical characteristics and evolution of hot fluids in the Gudui geothermal field in Comei County, Himalayas[J]. Geothermics, 81: 243-258. doi: 10.1016/j.geothermics.2019.05.010

    CrossRef Google Scholar

    [25] 王贵玲, 刘彦广, 朱喜, 等, 2020. 中国地热资源现状及发展趋势[J]. 地学前缘, 27（1）: 1-9

    Google Scholar

    Wang G L, Liu Y G, Zhu X, et al. , 2020. The status and development trend of geothermal resources in China[J]. Earth Science Frontiers, 27（l）: 1-9.

    Google Scholar

    [26] Wang P, Chen X H, Shen L C, et al. , 2016. Geochemical features of the geothermal fluids from the Mapamyum non-volcanic geothermal system （Western Tibet, China）[J]. Journal of Volcanology and Geothermal Research, 320: 29-39. doi: 10.1016/j.jvolgeores.2016.04.002

    CrossRef Google Scholar

    [27] 余浩文, 刘昭, 荣峰, 等, 2021. 西藏错那地热田水化学特征与物源机制[J]. 地质科技通报, 40（3）: 34-44

    Google Scholar

    Yu H W, Liu Z, Rong F, et al. , 2021. Characteristics and source mechanism of geothermal field in Cuona, Tibet[J]. Bulletin of Geological Science and Technology, 40（3）: 34-44.

    Google Scholar

    [28] Yuan J F, Guo Q H and Wang Y X, 2014. Geochemical behaviors of boron and its isotopes in aqueous environment of the Yangbajing and Yangyi geothermal fields, Tibet, China[J]. Journal of Geochemical Exploration, 140: 11-22. doi: 10.1016/j.gexplo.2014.01.006

    CrossRef Google Scholar

    [29] 张朝锋, 史强林, 张玲娟, 2018. 青藏高原新生代岩浆活动与地热关系探讨[J]. 中国地质调查, 5（2）: 18-24

    Google Scholar

    Zhang C F, Shi Q L, Zhang L J, 2018. Discussion on the relationship between Cenozoic magmatic activity and geotherm in Tibetan Plateau[J]. Geological Survey of China, 5（2）: 18-24.

    Google Scholar

    [30] 张梦昭, 郭清海, 刘明亮, 等, 2023. 山西忻州盆地地热水地球化学特征及其成因机制[J]. 地球科学, 48（3）: 973-987

    Google Scholar

    Zhang M Z, Guo Q H, Liu M L, et al. , 2023. Geochemical characteristics and formation mechanism of geothermal waters in the Xinzhou Basin, Shanxi Province[J]. Earth Science, 48（3）: 973-987.

    Google Scholar

    [31] 张彦鹏, 黎清华, 余绍文, 2022. 海南岛东海岸官塘地区地热水水化学特征及其循环演化过程识别[OJ]. 地球科学: 1 − 22

    Google Scholar

    Zhang Y P, Li Q H, Yu S W, 2022. Hydrochemical characteristics constrain on evolution of geothermal water in Guantang area in the east coast of Hainan Island [OJ]. Earth Science: 1 − 22.

    Google Scholar

    [32] 张云辉, 2018. 鲜水河断裂康定−磨西段地热系统成因及开发利用研究[D]. 成都: 成都理工大学.

    Google Scholar

    Zhang Y H, 2018. Research on genesis and development of the geothermal system in the Kangding−Moxi segment of the Xianshuihe fault[D]. Chengdu: Chengdu University of Technology.

    Google Scholar

    [33] 赵斌, 吕玥, 温柔, 等, 2023. 西藏地热能开发利用现状及发展前景[J]. 热力发电, 52（1）: 1-6

    Google Scholar

    Zhao B, Lv Y, Wen R, et al. , 2023. Utilization situation and development prospect of geothermal energy in Tibet[J]. Thermal Power Generation, 52（1）: 1-6.

    Google Scholar

    [34] 赵平, Mack K, 多吉, 等, 2001. 西藏羊八井热田地热流体成因及演化的惰性气体制约[J]. 岩石学报, 17（3）: 497 − 503

    Google Scholar

    Zhao P, Mack K, Duo J, et al. , 2001. Noble gases constraints on the origin and evolution of geothermal fluids from the Yangbajain geothermal field, Tibet. Acta Petrologica Sinica, 17（3）: 497 − 503.

    Google Scholar

    [35] 赵平, 金建, 张海政, 等, 1998. 西藏羊八井地热田热水的化学组成[J]. 地质科学, 33（1）: 62 − 73.

    Google Scholar

    Zhao P, Jin J, Zhang H Z, et al., 1998. Chemical composition of thermal water in the Yangbajing geothermal field, Tibet[J]. Scientia Geologica Sinica, 33（1）: 61 − 72.

    Google Scholar

    [36] 邹俊, 武斌, 马昭雄, 等, 2022. 西藏谢通门县卡嘎地热成因与资源潜力分析[OJ]. 水文地质工程地质: 1 − 10

    Google Scholar

    Zou J, Wu B, Ma Z X, et al. , 2022. Geothermal Origin and Resource Potential of Kaga in Xietongmen County, Tibet[OJ]. Hydrogeology & Engineering Geology: 1 − 10.

    Google Scholar

    • Relative Articles
  • Cited by
  • Supplements
    • Proportional views
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Figures(9)

Export Citation
PDF
XML

Article Metrics

Article views(1089) PDF downloads(184) Cited by(0)

Access History

Other Articles By Authors

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    版权所有：中国地质调查局发展研究中心 copyright @2020