ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
中国大陆主要地质构造单元岩石圈地热特征
  
关键词:heat flow  heat production rate of the crust  effective elastic thickness  China Mainland
基金项目:国家自然科学基金重点项目(No.49733110),中国博士后科学基金,人事部博士后经费资助,中国地质调查局国土资源大调查
作者单位
汪洋 中国地质大学(北京)地质矿产系北京 
汪集旸 中国科学院地质与地球物理研究所北京 
熊亮萍 中国科学院地质与地球物理研究所北京 
邓晋福 中国地质大学(北京)地质矿产系北京 
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摘要:
Lithospheric Geothermics of Major Geotectonic Units in China Mainland
      Lithospheric geothermal characteristics of major geotectonic units in China were studied on the basis of over 800 heat flow data from China Mainland. The spatial pattern of heat flow and other thermal parameters of lithosphere show obvious lateral variations, which originated from the Cenozoic tectonothermal activities related to the India-Asia collision and the subduction of the Pacific Plate. The average heat production rate of the crust also exhibits lateral heterogeneity among geotectonic units, implying significant lateral variation of bulk composition of the crust in China Mainland. The mechanical strength of the crust and the seismicity of geotectonic units were strongly affected by geothermal characteristics of the units.
WANG Yang,WANG Qi-yang,XIONG Liang-ping,DENG Jin-fu.2001.Lithospheric Geothermics of Major Geotectonic Units in China Mainland[J].Acta Geoscientica Sinica,22(1):17-22.
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