| 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.邯郸市东部平原区地热地质条件初析[J].地球学报,2000,21(2):177-181. |
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| 作者姓名： | 袁同星 刘东生 |
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| 作者单位： | 中煤第一勘探局,河北邯郸;邯郸市地质矿产局 |
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| 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。
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| 关 键 词： | 地热地质条件 热储层 邯郸市东部平原 |
A Preliminary Discussion Analysis of Geotherm-Geological Conditions in the Eastern Plain of Handan City |
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| YUAN Tong-xing and LIU Dong-sheng.A Preliminary Discussion Analysis of Geotherm-Geological Conditions in the Eastern Plain of Handan City[J].Acta Geoscientia Sinica,2000,21(2):177-181. |
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| Authors: | YUAN Tong-xing and LIU Dong-sheng |
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| Institution: | No.1 Exploration Bureau, China Administration of Coal Geology, Handan, Hebei;Handan Institute of Geology and Mineral Resources |
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| Abstract: | |
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| Keywords: | geothermo-geological condition thermal reservoir eastern plain of Handan city |
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