Advanced Search

Indexed by SCI、CA、РЖ、PA、CSA、ZR、etc .

Volume 11 Issue 3
Sep 2000
Turn off MathJax
Article Contents
Yang Wang, Jiyang Wang, Jinfu Deng. Geothermal Characteristics and Geological Implications of Major Tectonic Units in China. Journal of Earth Science, 2000, 11(3): 346-351.
Citation: Yang Wang, Jiyang Wang, Jinfu Deng. Geothermal Characteristics and Geological Implications of Major Tectonic Units in China. Journal of Earth Science, 2000, 11(3): 346-351.

Geothermal Characteristics and Geological Implications of Major Tectonic Units in China

Funds:

PRC and the Project of National Natural Science Foundation of China 49733110

  • Received Date: 08 May 2000
  • Accepted Date: 16 May 2000
  • On the basis of more than 900 heat flow data in China and the surrounding seas, the authors study the geothermal characteristics of major tectonic units in China. The spatial pattern of heat flow and other thermal parameters for lithosphere exhibit significant lateral variation, originating from the Cenozoic tectonothermal activities related to the subduction of the Pacific plate and the collision between India and Asia. The mechanical strength of the crust and the seismicity of tectonic units were strongly affected by geothermal characteristics of units. The crustal heat production rate also shows the lateral heterogeneity, implying the significant lateral variation of bulk composition of the crust in China.

     

  • loading
  • Burov E, Diament M, 1995. The Effective Elastic Thickness of Continental Lithosphere: What Does It Really Mean? JGR, 100: 3905-3927 doi: 10.1029/94JB02770
    Chapman D S, Furlong K P, 1992. Thermal State of the Continental Lower Crust. In: Fountain D M, Arculus R, Kay R W, eds. Continental Lower Crust. Amsterdam: Elsevier. 179-199
    Chapman D S, Pollack HN, 1975. Global Heat Flow: A New Look. Earth Planet Sci Lett, 28: 23-32 doi: 10.1016/0012-821X(75)90069-2
    Gao S, Luo T C, Zhang B R, et al, 1998. Chemical Composition of the Continental Crust as Revealed by Studies in East China. Geochimica et Cosmochimica Acta, 62: 1959-1975 doi: 10.1016/S0016-7037(98)00121-5
    Ito K, 1976. Heat Flow and Thickness of the Oceanic Lithosphere. Earth Planet Sci Lett, 30: 65-70 doi: 10.1016/0012-821X(76)90009-1
    Li T, 1994. The Abundance of Elements in Continental Crust, Upper Crust and Sedimentary Layer of China. Geochimica, 8: 140-145 (in Chinese with English Abstract)
    Li T, Ni S, 1997. Element Abundances of the Continental Lithosphere in China. Geology and Prospecting, 33: 31-37 (in Chinese with English Abstract)
    Li T, Ni S, 1998. Element Abundances of the Crust and Lithosphere in Tarim-North China Plate. Geology and Prospecting, 34: 20-24 (in Chinese with English Abstract)
    Li T, Yuan H, Wu S, et al, 1999. Regional Element Abundances of the Continental Crustobodies in China. Geotectonica et Metallogenia, 23: 101-107 (in Chinese with English Abstract)
    McLennan S M, Taylor S R, 1996. Heat Flow and the Chemical Composition of Continental Crust. J Geol, 104: 369-377 doi: 10.1086/629834
    Ni S, Man F, Wang Z, et al, 1999. Characteristics of Heat Production Distribution in Northern Xinjiang. Journal of University of Science and Technology of China, 24: 408-414 (in Chinese with English Abstract)
    Pollack H N, Hunter S J, Johnson J R, 1993. Heat Flow from the Earth' s Interior; Analysis of the Global Data Set. Rev Geophys, 31: 267-280 doi: 10.1029/93RG01249
    Ren J, 1999. The Geotectonic Map of China and Its Adjacent Area (1 ∶ 5 000 000). Beijing: Geological Publishing House
    Rudnick R L, McDonough W F, O' Connell R J, 1998. Thermal Structure, Thickness and Composition of Continental Lithosphere. Chemical Geology, 145: 395-411 doi: 10.1016/S0009-2541(97)00151-4
    Sengor A M C, 1999. Continental Interiors and Craton: Any Relation? Tectonophysics, 305: 1-42 doi: 10.1016/S0040-1951(99)00043-8
    Shi Y, Wang C, 1997. Thermal Modeling of the Formation of Leucogranite in the Higher Himalaya. Acta Geophysica Sinica, 40: 667-676 (in Chinese with English Abstract)
    Stein C, Stein S, 1992. A Model for the Global Variation in Oceanic Depth and Heat Flow with Lithospheric Age. Nature, 359: 123-129 doi: 10.1038/359123a0
    Vauchez A, Tommasi A, Barruol G, 1998. Rheological Heterogeneity, Mechanical Anisotropy and Deformation of the Continental Lithosphere. Tectonophysics, 296: 61-86 https://www.sciencedirect.com/science/article/pii/S0040195198001371
    Wang J, Huang S, 1990. Compilation of Heat Flow Data in the China Continental Area. 2nd ed. Seismology and Geology, 12: 351-366 (in Chinese and English Abstract)
    Wang Y, 1999a. An Analysis for Continental Heat Flow in China: [Dissertation]. Beijing: Institute of Geology, Chinese Academy of Sciences. 118 (in Chinese with English Abstract)
    Wang Y, 1999b. The Relationship between Helium Isotope Composition in Underground Fluid and the Crust/Mantle Ratio of Continental Heat Flow. In: Annual of the Chinese Geophysical Society 1999. Hefei: Anhui Science and Technology Press. 320 (in Chinese)
    Wang Y, 1999c. A Study on Mantle Heat Flow of Continental Area of China by Helium Isotope Ratio of the Underground Fluid. Acta Geoscientia Sinica— Bulletin of the Chinese Academy of Geological Sciences, 20(Suppl): 48-50 (in Chinese with English Abstract)
  • 加载中

Catalog

    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

    Tables(5)

    Article Metrics

    Article views(250) PDF downloads(23) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return