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Mineralogical and Paragenic Relalion Study of Fluorite in the Granite-related Uranium Deposits
作者姓名:GUO Yuping  SONG Hao  NIE Rui  LI Qi  YAN Wenquan  SI Fei  ZHAO Zichao  YAO Chang  LI Wei
摘    要:


Characteristics of Temperature Distribution and Control factors in Geothermal Field
Authors:GUO Yuping  SONG Hao  NIE Rui  LI Qi  YAN Wenquan  SI Fei  ZHAO Zichao  YAO Chang  LI Wei
Institution:1 Chengdu University of Technology, Chengdu 610059, Sichuan, China,1 Chengdu University of Technology, Chengdu 610059, Sichuan, China 2 Key Laboratory of Uranium Geology, China Geological Survey, Tianjin 300170, China 3 Key Laboratory of Radioactive and Rare Scattered Minerals, Ministry of Land and Resources, Guangzhou 512026, Guangdong, China,1 Chengdu University of Technology, Chengdu 610059, Sichuan, China,1 Chengdu University of Technology, Chengdu 610059, Sichuan, China,1 Chengdu University of Technology, Chengdu 610059, Sichuan, China,1 Chengdu University of Technology, Chengdu 610059, Sichuan, China,1 Chengdu University of Technology, Chengdu 610059, Sichuan, China,1 Chengdu University of Technology, Chengdu 610059, Sichuan, China and 1 Chengdu University of Technology, Chengdu 610059, Sichuan, China
Abstract:In recent years, China has carried out large‐scale exploration, exploitation and utilization of geothermal resources, but there is no unified understanding of the distribution characteristics of geothermal field and the controlling factors of forming geothermal field. As for the heat source, some scholars think it is the contribution of radioactivity, fault, magma chamber, or an abnormal heat source, and even the heat generated by the influence of the tectonic movement. As a result, many exemplary geothermal explorations have made great mistakes. After drilling at a depth of 3000‐5000m, the temperature obtained is not as good as the common low‐temperature sedimentary basin, and the losses are huge and extremely uneconomical.
Keywords:Geothermal desserts  heat conduction  tectonic movement  new energy  magma chamber zoic in China  Mafic and ultramafic magma derived from deep mantle
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