收稿日期: 2000-12-27
网络出版日期: 2001-01-10
基金资助
国家自然科学基金 ( 49733110 ;49772 15 5 )“中国花岗岩与大陆地壳生长”重点项目 ;国土资源部科技发展计划 ;中国博士后科学基金 ( 2 0 0 0 10 10 2 0 2 ;2 0 0 0 10 10 2 0 6) ;国家攀登专项 (SSER III 2 );人事部博士后经费联合资助项目
Terrestrial Heat Flow Pattern and Thermo tectonic Domains in the Continental Area of China
Received date: 2000-12-27
Online published: 2001-01-10
汪洋 , 邓晋福 , 汪集旸 , 熊亮萍 . 中国大陆热流分布特征及热-构造分区[J]. 中国科学院大学学报, 2001 , 18(1) : 51 -58 . DOI: 10.7523/j.issn.2095-6134.2001.1.009
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.
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