摘要
云南保山盆地是典型断陷盆地,众多温泉沿断层带出露,推断该盆地热源为地慢热流,热通道为盆地边缘的大断裂,盆地新近系、第四系粘土质岩等为地热良好的热储盖层,盆地地处高热流区,保山盆地具有较好的热源、热通道、热储盖层条件,地热开发前景良好。
Baoshan basin is a typical fauh basin in Yunnan. There are a lot of hot springs along the fault zone. We believe that the heat source is derived from the mantle thermal fluid. The megafauh of basin margin is the channel of thermal fluid. The good reservoir and cover bed of geotherm are Neogene, Quaternary claystone, etc. The basin is an area of high geotherm fluid. The potentiality of geotherm development in Baoshan basin is good because of the good geotherm source, heat channel, reservoir and cover beds.
出处
《云南地质》
2015年第2期176-180,共5页
Yunnan Geology
关键词
断陷盆地
地慢热源:断裂热通道
云南保山
Fault Basin
Mantle Heat Source
Fault Heat Channel
Baoshan, Yunnan
