The metallogenic regularity, development and utilization of peat deposits in China

被引：0
|
作者：
Rao J. [1 ,2 ]
Jia Q. [3 ]
Wang D. [2 ]
Liu L. [2 ,4 ]
Dai H. [2 ]
Guo W. [2 ]
机构：
[1] China University of Geosciences (Beijing), Beijing
[2] MNR Key Laboratory of Metallageny and Mineral Assessment, Institude of Mineral Resources, CAGS, Beijing
[3] MLR Key Laboratory of Saline Lake Resources and Environments, Institute of Mineral Resources, CAGS, Beijing
[4] Geology and Mineral Resources Scientific Institute of Sichuan Exploration Bureau of Geology and Mineral Resources, Chengdu
来源：
Dizhi Xuebao/Acta Geologica Sinica | 2020年 / 94卷 / 01期
关键词：
Metallogenic regularities; Non-metallic mineral; Ore-concentration area; Peat; Utilization trend;
D O I：
10.19762/j.cnki.dizhixuebao.2020128
中图分类号：
学科分类号：
摘要：
Peat is an emerging industrial mineral of great significance, and a typical example of "gorgeous turn" from traditional minerals to emerging industries. Globally a total of 500 billion tons of peat is consumed of which China's share is 12.496 billion tonsof rich and medium-quality peat with a rising demand. The metallogenic epoch developed during the Quaternary (Holocene), when most of the peat was converted to lignite. The main type of peat deposits in China are eutrophic meadow peat, followed by woody peat and moss peat in the second and third place. Metallogenic regularities summarized in this paper are based on a review of 5719 peat deposits listed in the 1988 National peat report. Five large-scale ore-concentrated areas, seven small and medium-sized ore-concentrated areas, and three large-scale prediction area are plotted based on available knowledge, thus providing a theoretical framework for the exploration of peat resources. A fresh survey is now necessary as many peatlands identified in the last national survey thirty years ago have disappeared due to global climate change, urbanization and other reasons. It is important to emphasize that the importance of peat is no longer limited to fuel, but is also relevant for energy conservation, ecosystem and environmental protection, as a carbon sink and in biotechnology. With this in view, the editorial board of China Mineral Geology has recommended that peat be classified as a non-metallic mineral and invited suggestions for its development and utilization. © 2020, Science Press. All right reserved.
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页码：192 / 203
页数：11
相关论文
共 56 条
  • [1] Aldmour S.T., Burke I.T., Bray A.W., Baker D.L., Ross A.B., Gill F.L., Cibin G., Ries M.E., Stewart D.I., Abiotic reduction of Cr (VI) by humic acids derived from peat and lignite: kinetics and removal mechanism, Environmental Science and Pollution Research, 26, 5, pp. 4717-4729, (2019)
  • [2] Andersen R., Farrell C., Graf M., Muller F., Anderson P., An overview of the progress and challenges of peatland restoration in western Europe, Restoration Ecology, 25, 2, pp. 271-282, (2016)
  • [3] Chai X., The formation and types of peat in China and the law of govering its distribution, Acta Geographica Sinica, 36, 3, pp. 237-253, (1981)
  • [4] Chen H., Yang G., Peng C., Zhang Y., Zhu D., Zhu Q., Hu J., Wang M., Zhan W., Zhu E., The carbon stock of alpine peatlands on the Qinghai-Tibetan Plateau during the Holocene and their future fate, Quaternary Science Reviews, 95, pp. 151-158, (2014)
  • [5] Chen S., Jin S., The qualities and using prospects for herbaceous peat in China, Journal of Northeast Normal University, 2, pp. 93-103, (1984)
  • [6] Chen Y., Zhu Y., Xiao K., Zhang X., Mei Y., Yan S., Liu Y., Song G., Li C., Wang Y., Dong J., Li H., Dong J., Division of minerogenic provinces (belts) in China, Mineral Deposits, 25, pp. 1-6, (2006)
  • [7] Chen Y., Wang D., Zhu Y., Xu Z., Ren J., Zhai Y., Chang Y., Tang Z., Pei R., Teng J., Deng J., Hu Y., Ren T., Shen B., Wang S., Xiao K., Peng R., Qian Z., Mei Y., Du J., Shi J., Zhang X., Zhu M., Xu J., Xue C., Chinese Mineralization System and Assessment of Regional Mineralization, (2007)
  • [8] Dai L., Actively carry out geological survey of peat resources, Geology in China, 7, pp. 9-11, (1984)
  • [9] Dean S.A., Tobin J.M., Uptake of chromium cations and anions by milled peat, Resources Conservation & Recycling, 27, 1-2, pp. 151-156, (1999)
  • [10] Dieleman C.M., Lindo Z., McLaughlin J.W., Craig A.E., Branfireun B.A., Climate change effects on peatland decomposition and porewater dissolved organic carbon biogeochemistry, Biogeochemistry, 128, 3, pp. 385-396, (2016)
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