摘要
玉溪北城地区地热为活动性深大断裂导热类型,地热分布于沿普渡河断裂的南延部分,隐伏于玉溪盆地北部地段。分析地下热水形成机理及开发。
The geothermal water of Beicheng area in Yuxi belongs to the heat transfer type of active megafault. The geothermal water is distributed in the S - extension part of Puduhe fault and buried under the N part of Yuxi basin. In this paper, we have an analysis of the formation mechanism of geothermal water.
出处
《云南地质》
2011年第3期357-361,共5页
Yunnan Geology
关键词
北城地热
导热断裂
良好含水层
良好保温盖层
云南玉溪北城
Beicheng Geothermal Water
Fault of Heat Transfer
Good Water- Bearing Bed
Good Insu-lation Cover
Beicheng, Yuxi, Yunnan
