| 邯郸市东部平原区地热地质条件初析 |
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| 引用本文：袁同星,刘东生.2000.邯郸市东部平原区地热地质条件初析[J].地球学报,21(2):177-181. |
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| 中文摘要:邯郸市东部平原区属华北平原冀南坳陷 ,新生界厚度约 1500m。热储层为上第三系馆陶组和明化镇组下部砂砾岩含水层。地热类型为受上地幔传导热流加热的盆地边缘水热型层状温热水。根据地热地质条件及邻区地热信息和地温梯度 ,邯郸市东部平原区有望找到50～58℃以上的温热水。 |
| 中文关键词:地热地质条件 热储层 邯郸市东部平原 |
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| A Preliminary Discussion Analysis of Geotherm-Geological Conditions in the Eastern Plain of Handan City |
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| Abstract:The eastern plain of Handan city belongs to the south Hebei depression.The Cenozoic is about 1 500m in depth. The thermal reservoir includes sand-gravel aquifer of Guantao Formation and the bottom of Minghuazhen Formation of Neogene.The geothermal resource is of stratified hot water type at the margin of the basin,which was heated by the conduction heat. According to geothermal and geological conditions,geothermal information and geothermal gradient of adjacent areas,the conclusion can be drawn that there exists the possibility of finding hot water of 51～58℃ in the eastern plain of Handan. |
| keywords:geothermo-geological condition thermal reservoir eastern plain of Handan city |
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