|
|||||
|
|
| 云南腾冲地区现代地热流体活动类型 | |
| 引用本文： | 上官志冠,孙明良,李恒忠.云南腾冲地区现代地热流体活动类型[J].地震地质,1999,21(4):436-442. |
| 作者姓名： | 上官志冠 孙明良 李恒忠 |
| 作者单位： | 1. 中国地震局地质研究所,北京,100029 2. 中国科学院兰州地质研究所,兰州,730000 3. 云南省腾冲县地震局,云南腾冲,679100 |
| 基金项目： | 国家地震局“九五”重点项目资助!(95110204) |
| 摘 要： | 腾冲地区存在两类地热流体活动。其中热海- 热水塘地区、马鞍山火山口附近的地热流体活动属火山区地热流体活动,其热源或气体挥发组分的物质来源与近代火山喷发活动或现代幔源岩浆侵入活动直接有关。区内其它地热流体活动多属构造活动成因。在腾冲地区,地热流体逸出He 的3 He/4 He≥1-2 Ra 可作为区别这两类地热流体的可靠指标 |
| 关 键 词： | 火山 地热 流体 氦同位素地球化学 |
| 修稿时间： | 1998年10月1日 |
ACTIVE TYPES OF MODERN GEOTHERMAL FLUIDS AT THE TENGCHONG REGION, YUNNAN PROVINCE |
|
| SHANGGUAN Zhiguan,Sun Mingliang,Li Hengzhong.ACTIVE TYPES OF MODERN GEOTHERMAL FLUIDS AT THE TENGCHONG REGION, YUNNAN PROVINCE[J].Seismology and Geology,1999,21(4):436-442. | |
| Authors: | SHANGGUAN Zhiguan Sun Mingliang Li Hengzhong |
| Abstract: | In the Tengchong region, there exist two kinds of active geothermal fluids. Only those active geothermal fluids distributed at the Rehai Reshuitang and nearby areas of the Maan shan crater really deserve to be called the volcanic geothermal fluids. It means that their thermal source or the volatile components escaped from the geothermal fluid could be related to the modern volcanic activity or magmatic intrusion. Other geothermal fluids are all generally the thermal discharge caused by the tectonic activi |
| Keywords: | Volcano Geotherm Fluid He isotopic geochemistry |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ | |
