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Terrestrial Heat Flow Pattern and Thermo tectonic Domains in the Continental Area of China

  • Wang Yang ,
  • Deng Jinfu ,
  • Wang Jiyang ,
  • Xiong Liangping
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  • 1. Division of Petrology, School of Earth Science and Resources, China University of Geosciences, Beijing 100083;

    2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029

Received date: 2000-12-27

  Online published: 2001-01-10

Abstract

On the basis of total 822 heat flow measurement in the continental area of China, the deep geothermal characteristics of lithosphere of the major tectonic units was studied, which includes the temperature at 40 km depth, the thickness of thermal lithosphere, the cumulated strength and effective elastic thickness (EET) of lithosphere and so on. The results exhibit significantly lateral heterogeneity for heat flow pattern, thermal state and rheological features of lithosphere in China, which resulted from the Cenozoic tectonothermal activities related to the Pacific subduction as well as the collision between India and Asia. According to heat flow values and deep geothermal characteristics, three large scale thermo tectonic domains, i.e. Eastern, Central and Western domain, can be identified in the continental area of China.

Cite this article

Wang Yang , Deng Jinfu , Wang Jiyang , Xiong Liangping . Terrestrial Heat Flow Pattern and Thermo tectonic Domains in the Continental Area of China[J]. Journal of University of Chinese Academy of Sciences, 2001 , 18(1) : 51 -58 . DOI: 10.7523/j.issn.2095-6134.2001.1.009

References

1 汪洋.中国大陆大地热流分析 :[ 博士学位论文].北京 :中国科学院地质研究所, 1999

2 汪洋, 汪集, 熊亮萍, 邓晋福.中国大陆及海域大地热流分布特征及岩石圈热结构.见 :中国地球物理学会 2000 年年刊.武汉 :中国地质大学出版社, 2000.259

3 Pollack H N, Hunter S J, Johnson J R.Heat Flow from the Earth' s Interior;A nalysis of the G lobal Data Set.Rev Geophys, 1993, 31:267 ~ 280

4 汪集, 黄少鹏.中国大陆地区大地热流数据汇编(第二版).地震地质, 1990, 12:351 ~ 366

5 任纪舜.中国及邻区大地构造图(1 :5 000 000).北京 :地质出版社, 1999

6 Shen P-Y, Wang K, Beck A E.Crustal Thermal Models Along East European G eotraverses:Inverse Solutions.Tectonophysi cs, 1991, 194 :363 ~ 385

7 Chapman D S, Furlong K P.Thermal St ate of the Continental Lower Crust.In :Fountain D M, Arculus R, K ay R W, eds.Continental Lower Crust.Amsterdam :Elsevier, 1992.179 ~ 199

8 石耀霖, 王其允.高喜马拉雅淡色花岗岩形成的热模拟.地球物理学报, 1997, 40:667 ~ 676

9 汪洋.对“新疆北部地区岩石生热率分布特征” 一文的商榷.中国科学技术大学学报, 2000, 30(5):627~ 632

10 Gao S, Zhang B-R, Jin Z-M, et al.How Mafic is the Lower Continental Crust.Earth Planet Sci Lett, 1998, 161:101 ~ 117

11 Burov E, Diament M.The Effective Elastic Thickness of Continental Lithosphere:What does it Really Mean ? J Geophys Res, 1995, 100:3905 ~3927

12 Chapman D S, Pollack H N.G lobal Heat Flow :A New Look.Earth Planet Sci Lett, 1975, 28 :23~ 32

13 王勇, 许厚泽.中国大陆及其邻区岩石层挠曲强度变化和均衡补偿机制.地球物理学报, 1996, 39(增刊):105 ~ 113

14 刘若新, 陈文寄, 孙建中, 李大明.中国新生代火山岩的 K-Ar 年代与构造环境.见 :刘若新主编.中国新生代火山岩年代学与地球化学.北京:地震出版社, 1992.1~ 43

15 叶加仁, 赵鹏大, 陆明德.鄂尔多斯盆地下古生界油气地质动力学研究.中国科学 D 辑, 2000, 30(1):40 ~ 46

16 石耀霖.地球的热演化与动力学过程.见 :现今地球动力学问题讨论会文集.北京 :地震出版社, 1994.37 ~ 45

17 邓万明, 孙宏娟.青藏高原新生代火山活动与高原隆升关系.地质论评, 1999, 45(suppl):952 ~ 958

18 Yin A, Harrison T M.Geological Evolution of the Himalayan-Tibet an Orogen.Annu Rev Earth Planet Sci, 2000, 28 :211 ~ 280

19 McNamara D E, Owens T J, Silver P G, Wu F T.Shear Wave A nisotropy Beneath the Tibetan Plateau.J Geophys Res, 1994, 99:13655 ~ 13665

20 Wei Wenbo, Tan Handong, Jin Sheng, et al.Electrical Structure of the Crust and Upper M ant le of Tibetan Plateau from Magnetotelluric Prof iling of INDEPTH-MT.地学前缘, 2000, 7(suppl)-15HKT abstract volume :319

21 Owens T J, Zandt G.Implications of Crustal Property Variations for Models of Tibetan Plateau Evolution.Nature, 1997, 387 :37 ~ 43

22 Wang Yang.Vp/ Vs Estimation in Tibet an Crust f rom Inversion of Surface Wave Dispersions.地学前缘, 2000, 7(suppl)-15HKT abstract volume :373

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