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Geothermal resources in Tibet of China: current status and prospective development

Environmental Earth Sciences volume 76, Article number: 239 (2017) Cite this article

Abstract

Tibet boasts many huge geothermal reserves and resource exploitation potential. However, as the geothermal resource is relatively scattered, it is hard to be exploited. The scope of work includes assessments of geothermal and ground water storage capacity, and the amount of exploitable heat and water and the fluid quality are evaluated in separate geothermal districts (fields) on the basis of the former investigation on geothermal wells, springs and geothermal field. Considering the low degree of general survey in Tibet and less information available, the amount of geothermal water in Tibet is calculated by natural heat flux method (SPA). The exploited amount of geothermal fluid (SPA) in Tibet mountainous area is 7.65 × 107 m3/a, and the exploitable geothermal resources (SPA) are 1700.77 × 1013 J/a, equivalent to 51.1 × 104 T of standard coal. A single interception of natural heat flow (SPA) shows that there is a huge potential for the development and utilization of geothermal resources in Tibet mountainous areas. Hot dry rock resources evaluation is conducted as well. Statistics show that this region’s base temperature is greater than 150 °C, and 19 zones are found with surface thermal fluid above boiling point. It is calculated that the thermal reserve 3–5 km below amounts to 145,367.93 × 1015 J, equivalent to 49.68 × 108 tons of standard coal. In south Tibet, the currently developed and utilized geothermal resources are mainly from Yangbajing thermal field. Early exploited amount of shallow geothermal resources amounts to 1512 t/h. Other geothermal active areas are basically unexploited. In middle Tibet, the geothermal active zones are still in natural forms without any exploitation. The total amount of geothermal liquid resources in north Tibet is 8.3 × 104 m3/a. East Tibet area’s geothermal resources are basically unexploited. The total amount of geothermal liquid resources is 3.77 × 105 m3/a. According to the results of geothermal resources evaluation in each area of Tibet, most geothermal active zones are in their natural state and not utilized, and are exploitation zones with high potential, especially in south and east Tibet uplifted zones.

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References

  • China Geological Survey (2014) The geothermal resource investigation and evaluation division technical requirements. Internal report

  • Geothermal and Geological Institute, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau (1984) Report on geothermal field resources of shallow geothermal reservoir of Yangbajing in Dangxiong County, Tibet Autonomous Region

  • Geothermal and Geological Institute, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau (1987) Geological report on detailed inspection on Naqu geothermal field in Naqu County, Tibet Autonomous Region

  • Geothermal and Geological Institute, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau (1991) Geothermal resource regionalisation in Tibet Autonomous Region. Internal report

  • Geothermal and Geological Institute, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau (1995a) Geological report on general inspection on gothermal resources of North Yangbajing geothermal field in Dangxiong County, Tibet Autonomous Region

  • Geothermal and Geological Institute, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau (1995b) Hydrogeological report on general inspection on geochemistry study of high temperature thermal fluid in Tibet Autonomous Region

  • Geothermal and Geological Institute, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau (2015) Tibetan geothermal resources evaluation and regionalisation research report

  • Institute of Geochemistry, Chinese Academy of Sciences, Guiyang (1977) Concise geochemical manual. Science Press

  • Jin C, Zhou Y (1978) The magmatic rock zone in Himalayan mountains and Gangdise arc mountains and the genetic models. Geol Sci 13(4):297–312

  • Liao Z (1988) Yunnan–Burma–Thailand tectonic domain and special cenozoic volcanic activity. J Peking Univ (Nat Sci Edn)(4):111–120

  • Liao Z, Zhao P (1999) Yunnan-Tibet geothermal belt: geothermal resources and typical geothermal system. Science Press, Beijing

    Google Scholar 

  • Lin W, Liu Z, Wang W, Wang G (2013) Geothermal resources and potential evaluation in China. Geol China 40(1):312–321

    Google Scholar 

  • Liu Y, Wang Q, Wu C (1977) Crustal structure and geological significance in the central region of Himalayan mountains. Chin J Geophys 20:143–149

    Google Scholar 

  • Pan Y, Wang Y, Chang C (1980) Evidence of Himalayan tectonic activity and Qinghai–Tibet plateau formation model. Seismol Geol 2:1–10

    Google Scholar 

  • Pan G et al (2012) Tectonic evolution of the Qinghai–Tibet plateau. J Asian Earth Sci 53:3–14. doi:10.1016/j.jseaes.2011.12.018

    Article  Google Scholar 

  • Roy RF, Blackwell DD, Birch F (1968) Heat generation of plutonic rocks and continental heat flow provinces. Earth Planet Sci Lett 5:1–12. doi:10.1016/S0012-821X(68)80002-0

    Article  Google Scholar 

  • Sandong Z, Wang D (1980) The seismic activity around the Himalayas. Seism Geol Transl (2):3–8

  • The Geological and Mineral of the People’s Republic of China (1985) Method for geothermal resource assessment

  • The Tibet Autonomous Region Geological Survey Institute (2009) Geothermal resource evaluation and regionalization in Tibet

  • Tian T, Li M, Bai Y (2006) Geothermal resources development and utilization in China. China Environmental Science Press, Beijing

    Google Scholar 

  • Toksöz MN, Bird P (1977) Modelling of temperatures in continental convergence zones. Tectonophysics 41:181–193

    Article  Google Scholar 

  • Tong W, Zhang M, Zhang Z (1981) Geothermal in Tibet. Science Press, Beijing

    Google Scholar 

  • Wei W et al (1997) Magnetotelluric deep exploration of the Tibetan plateau—crust–mantle electrical structure in Yadong–Bamucuo area. Modern Geol 11(3):366–374

    Google Scholar 

  • Xu Z, Yang J, Li H, Ji S, Zhang Z, Liu Y (2011) On the tectonics of the India–Asia collision. Acta Geol Sin 1:1–33

    Google Scholar 

  • Xu Z et al (2013) Three dimensional extrusion model of high Himalaya. Geol China 40(3):671–680

    Google Scholar 

  • Zhang Z, Li L (2005) China groundwater resources (Tibet part). China Cartographic Publishing House, Beijing

    Google Scholar 

  • Zhang X, Teng J, Sun R, Romanelli F, Zhang Z, Panza GF (2014) Structural model of the lithosphere–asthenosphere system beneath the Qinghai–Tibet plateau and its adjacent areas. Tectonophysics 634:208–226. doi:10.1016/j.tecto.2014.08.017

    Article  Google Scholar 

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Acknowledgements

This study was supported by grants from, geothermal evaluation and regionalization of China Geological Survey (Grant No. 12120113077300) and geothermal current status and regionalization of China Geological Survey (1212010818081). One of the authors was partially supported by the Fundamental Research Funds for central public research institutes (YK201501 and YK201611).

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Authors and Affiliations

  1. School of Water Resources and Environment, China University of Geosciences, Beijing, 100083, China

    Siqi Wang & Jingli Shao

  2. Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang, 050061, China

    Chuan Lu

  3. Geothermal and Geological Institute, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau, Lhasa, 850000, China

    Dawa Nan & Xiancai Hu

Authors
  1. Siqi Wang
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  2. Chuan Lu
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  3. Dawa Nan
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  4. Xiancai Hu
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  5. Jingli Shao
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Correspondence to Chuan Lu.

Additional information

This article is part of a Topical Collection in Environmental Earth Sciences on ‘‘Subsurface Energy Storage II’’, guest edited by Zhonghe Pang, Yanlong Kong, Haibing Shao, and Olaf Kolditz.

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Wang, S., Lu, C., Nan, D. et al. Geothermal resources in Tibet of China: current status and prospective development. Environ Earth Sci 76, 239 (2017). https://doi.org/10.1007/s12665-017-6464-5

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  • DOI: https://doi.org/10.1007/s12665-017-6464-5

Keywords

  • Geothermal resources
  • Tibet
  • Current status
  • Development
  • Potential