物探与化探2011，Vol.35Issue(1)：58-60,64,4.
地热田温度预测的反演电阻率方法
THE PREDICTION OF THE GEOTHERMAL FIELD TEMPERATURE BY MEANS OF RESISTIVITY INVERSION
孟银生 1姚长利 2刘瑞德 1黄力军2
作者信息
- 1. 中国地质大学地下信息探测技术与仪器教育部重点实验室,北京,100083
- 2. 中国地质科学院地球物理地球化学勘查研究所,河北,廊坊,065000
- 折叠
摘要
Abstract
The resistivity inversod by the CSAMT method can be used to detect the depth of the strata and deduce the spatial distribution of faults, and even predict the temperature of the thermal structure in some cases. Based on a discussion of the relationship between the underground temperature and the resistivity of the structure, this paper demonstrated the use of the distribution of resistivity inversion to predict the temperature of the geothermal field under certain conditions( with the consideration of the logging data), and the application results show the effectiveness of the technique.关键词
可控源音频大地电磁/反演电阻率/地热田/温度预测/热储构造分类
天文与地球科学引用本文复制引用
孟银生,姚长利,刘瑞德,黄力军..地热田温度预测的反演电阻率方法[J].物探与化探,2011,35(1):58-60,64,4.
