ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
地幔热柱演化及其地热效应——华北地热异常的深部构造背景
  
关键词:geothermal anomaly  mantle plume  submantle plume  graben and horst  north China downfaulted basin
基金项目:地矿部“百名跨世纪科技人才培养计划”项目资助
作者单位
孙爱群 石家庄经济学院 
牛树银 石家庄经济学院 
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摘要:
The Mantle Plume Evolution and Its Geothermal Effect--Deep Tectonic Setting of Geothermal Anomaly in North China
      Based on an analysis of characteristics and distribution regularities of geothermal anomalies as well as controlling factors of geothermal resources in north China basin,the authors hold that the uplifting of giant submantle plume is the main dynamic (thermal energy) source responsible for the crustal splitting, the formation and development of faulted depressions,and the evolution of geothermal field in north China. It is considered that the second-order uplifts and depressions in north China fault basin that led to geothermal gradient zoning are forms of tectonic control of geothermal resources.
SUN Ai-qun,NIU Shu-yin.2000.The Mantle Plume Evolution and Its Geothermal Effect--Deep Tectonic Setting of Geothermal Anomaly in North China[J].Acta Geoscientica Sinica,21(2):182-189.
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