摘要
云南地热异常多且显著。滇西高温水热活动区是藏滇水热带的南延,滇东断陷盆地中低温水热活动区的形成得益于独特的地质结构,滇西、滇南花岗岩地热系统则主要吸收地层中K40同位素放射热而成。开发前景极为广阔。
The geothermal anomaly is very evident in Yunnan. The high tempera - ture hydrothermal activity area in West Yunnan is the south extension of Xizang - Yunnan geothermal zone. The formation of middle - low temperature hydrothermal activity area in East Yunnan faulted basin is resulted from the distinct geological structure. The granite geothermal system in West Yunnan and South Yunnan is formed by the absorption of radioactive heat of K^40 isotope in rock bed. The development potentiality is very broad.
出处
《云南地质》
2006年第1期70-75,共6页
Yunnan Geology
关键词
热储层
热源
地热系统
地热水资源开发
云南
Geothermal System
Heat Source
Geothermal Reservoir
Development of Hydrothermal Resources
