| 高晓,景金明,杨书民,孙越英.济源市省庄地热区地质条件及成因特征[J].地质找矿论丛,2007,(3):228-231 |
| 济源市省庄地热区地质条件及成因特征 |
| GEOLOGICAL CONDITION AND GENETIC CHARACTERISTIC OF SHENGZHUANG GEOTHERMAL FIELD IN JIYUAN CITY,HENAN PROVINCE |
| 投稿时间：2006-11-27 修订日期：2007-05-08 |
| DOI：10.6053/j.issn.1001-1412.2007.3. 013 |
| 中文关键词: 地热资源 地质条件 成因特征 开发利用 济源市 河南省 |
| 英文关键词:geothermal resources geological condition genetic characteristic development and utilization Jiyuan city Henan province |
| 基金项目: |
| 作者 | 单位 | | 高晓 | 河南省地质矿产勘查开发局, 第二地质队, 河南, 焦作, 454002 | | 景金明 | 河南省地质矿产勘查开发局, 第二地质队, 河南, 焦作, 454002 | | 杨书民 | 河南省地质矿产勘查开发局, 第二地质队, 河南, 焦作, 454002 | | 孙越英 | 河南省地质矿产勘查开发局, 第二地质队, 河南, 焦作, 454002 |
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| 中文摘要: |
| 济源市省庄地热属于异常增温热水型及干热岩型地热区,是中国北方非火山岩浆岩区地热异常的典型地热区,地热水是大气降水通过盘古寺深大断层深循环的结果。地热分布受盘古寺断层、五龙口断层及次级断层的控制,并在断层交汇部位显示温度异常。热源来自于北部山区补给沿断层径流的深循环水。深循环水水温较高,与浅部受大气降水及地表水补给的冷水相混合。 |
| 英文摘要: |
| The Shengzhuang geothermal field is the dry-heat rock and abruptly-temperature-raised hot water type geothermal field and is the typical non-volcanic-magmatic geothermal anomaly area in the north China.The geothermal water is resulted from circulation of meteoric water in the Pangushi deep fault and the geothermal distribution is controlled by Pangushi,Wulongkou faults and the sub-faults and intersections of the faults confine the distribution of anomaly temperature.The heat energy comes from the circulating deeply water supplied from the northern mountainous area running off fault.The circulating water with relatively high temperature is mixed with cold water supplied from meteoric and surface water. |
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