| 南襄盆地南阳凹陷地热成因研究 |
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| 引用本文： | 原伟强,符勇.南襄盆地南阳凹陷地热成因研究[J].地下水,2011(1):27-28,38. |
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| 作者姓名： | 原伟强 符勇 |
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| 作者单位： | 河南理工大学; |
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| 摘 要： | 通过研究南阳凹陷区域地质构造,地温场特征和热储层特征,认为南阳凹陷地热田为典型的沉积盆地型地热田.南阳凹陷热源主要由地下水在正常梯度下经围岩增温加热和地下水沿深大断裂的上涌两部分组成,朱阳关——夏馆——大河断裂、方城——邓县断裂、新野断裂等活动性深大断裂为热量传导提供了良好的通道,古近系稳定的砂岩泥岩互层为深层地热良好...
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| 关 键 词： | 南阳凹陷 地温场 热储层 热源 导热通道 盖层 |
Research on the Geothermal Origin in Nanyang Depression,Nanxiang Basin |
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| YUAN Wei-qiang,FU Yong.Research on the Geothermal Origin in Nanyang Depression,Nanxiang Basin[J].Groundwater,2011(1):27-28,38. |
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| Authors: | YUAN Wei-qiang FU Yong |
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| Institution: | YUAN Wei-qiang,FU Yong(Henan Technology and Science University,Jiaozuo 454900,Henan) |
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| Abstract: | According to research on the regional geological structure of Nanyang depression,geothermal field characteristics and thermal reservoir characteristics,the article mentions that Nanyang depression geothermal field is a typical sedimentary basin geothermal field and is groundwater heated in the surrounding rock under normal gradient curtailing and groundwater upwelling along the deep fault is the main thermal source,Zhuyangguan-Xiaguan-Dahe fault,Fangcheng-Dengxian fault,Xinye fault,and such as these active ... |
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| Keywords: | Nanyang depression geothermal field thermal reservoir thermal source thermal conductive path and the cover |
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