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| 张家口地下热水资源成因探讨 | |
| 引用本文： | 魏洪章. 张家口地下热水资源成因探讨[J]. 中国煤田地质, 2006, 18(4): 38-41 |
| 作者姓名： | 魏洪章 |
| 作者单位： | 河北省煤田地质局第四地质队,河北宣化075100 |
| 摘 要： | 张家口地热资源丰富，通过对区内地热成矿机制，成矿规律的分析认为，以祁吕系为主的多构造体系复合部位控制了本区地下热水的形成与分布，本区地下热水是大气降水经深循环而成，经计算深循环的深度达为2600m，张家口南部地区有很多个热水异常点，是具有远景意义的地热区。 |
| 关 键 词： | 地热资源 成因探讨 构造体系 地温梯度 张家口 |
| 文章编号： | 1004-9177（2006）04-0038-04 |
A Discussion on Geothermal Resource in Zhangjiakou |
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| Wei Hongzhang. A Discussion on Geothermal Resource in Zhangjiakou[J]. Coal Geology of China, 2006, 18(4): 38-41 | |
| Authors: | Wei Hongzhang |
| Affiliation: | The 4th Geological Exploration Team, Hebei Bureau of Coal Geological Exploration, Xuanhua, Hebei 075100 |
| Abstract: | Zhangjiakou area has abundant geothermal resources. Through studies on geothermal genetic mechanism and pattern considered that the composite part of multi-tectonic systems predominately the Qilianshan-Luliangshan-Helanshan epsilon structural system controls the forming and distributing of geothermal water in the area, The geothermal water in the area is formed through the deep circulation of atmospheric precipitation and the calculated depth of circulation is amount to 2600m. There are many geothermal water anomalies in the southern part of Zhangjiakou, therefore is a prospect geothermal resource region. |
| Keywords: | geothermal resource discussion on genesis tectonic system geothermal gradient Zhangjiakou |
| 本文献已被 CNKI 维普 等数据库收录！ | |