High-Temperature Geothermal Source in the Northeastern Datong Basin,North China:Evidence from the Drilled Rhyolite  

作　　者：Dongdong Yuan Qiang Liu Haijin Xu Changsheng Zhang Daozhi An Meihua Wei Gaojing Ren 

机构地区：[1]School of Earth Sciences,School of Sustainable Energy,China University of Geosciences,Wuhan 430074,China [2]Shanxi Geological Engineering Exploration Institute Co.Ltd,Taiyuan 030024,China

出　　处：《Journal of Earth Science》2024年第5期1776-1780,共5页地球科学学刊（英文版）

摘　　要：0 INTRODUCTION The high-temperature(HT)geothermal resources from the earth interior have been considered as a kind of clean and regenerated energy to resolve the growing issues of energy consumption and environmental pollution(e.g.,Lund et al.,2022).Based on the geological background and forming mechanism,geothermal resources are commonly divided into the shallow,hydrothermal,dry hot rock and magmatic types(e.g.,Zhang et al.,2024;Mao et al.,2019).

关 键 词：EASTERN SHALLOW ROCK 

分 类 号：P314[天文地球—固体地球物理学]