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- 英文篇名：ASSESSMENT OF GEOTHERMAL POTENTIAL IN THE HEFEI AREA</li><li>中文刊名：<a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=%e5%ae%89%e5%be%bd%e5%9c%b0%e8%b4%a8">安徽地质</a></li><li>英文刊名：<a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=Geology+of+Anhui">Geology of Anhui</a></li><li>作者：<a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=%e5%ae%81%e9%87%91%e9%87%8e">宁金野</a> ; <a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=%e5%be%90%e6%b4%aa%e8%8b%97"><font color="red">徐洪苗</font></a></li><li>英文作者：<a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=NING+Jin-ye">NING Jin-ye</a> ; <a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=XU+Hong-miao(No.327+Geological+Party+of+Bureau+of+Geology+and+Mineral+Exploration">XU Hong-miao(No.327 Geological Party of Bureau of Geology and Mineral Exploration</a> ; <a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=Hefei">Hefei</a> ; <a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=Anhui+230011">Anhui 230011</a> ; <a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=China)">China)</a></li><li>中文关键词：<a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=%e5%9f%ba%e5%ba%95%e9%9a%86%e8%b5%b7%e8%81%9a%e7%83%ad%e5%9e%8b%e5%9c%b0%e7%83%ad%e5%9c%b0%e8%b4%a8%e6%88%90%e5%9b%a0%e6%a8%a1%e5%bc%8f">基底隆起聚热型地热地质成因模式</a> ; <a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=%e6%b8%85%e6%b4%81%e5%9c%b0%e7%83%ad%e8%83%bd%e6%ba%90">清洁地热能源</a> ; <a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=%e5%a4%a7%e5%9c%b0%e6%9e%84%e9%80%a0%e7%8e%af%e5%a2%83">大地构造环境</a> ; <a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=%e6%b7%b1%e9%83%a8%e5%9c%b0%e5%a3%b3%e7%bb%93%e6%9e%84">深部地壳结构</a> ; <a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=%e8%8e%ab%e9%9c%8d%e9%9d%a2%e9%9a%86%e8%b5%b7">莫霍面隆起</a> ; <a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=%e7%83%ad%e6%b5%81">热流</a></li><li>英文关键词：<a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=basement+uplift-caused+thermal+accumulation+geological+genesis+model">basement uplift-caused thermal accumulation geological genesis model</a> ; <a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=clean+geothermal+energy">clean geothermal energy</a> ; <a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=tectonic+setting">tectonic setting</a> ; <a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=deep+crustal+structure">deep crustal structure</a> ; <a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=Moho+surface+rise">Moho surface rise</a> ; <a target="_blank" href="/auto/db/search.aspx?db=950023&agfi=0&cls=0&uni=True&cid=0&gp=15&showgp=False&prec=False&md=299&pd=4&msd=293&psd=201&mdd=299&pdd=4&count=10&wrd=heat+flow">heat flow</a></li><li>出版日期：2011-03-15</li><li>机构：安徽省地质矿产勘查局327地质队;</li><li>年：2011</li><li>期：01</li><li>出版单位：安徽地质</li></ul></td>
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摘要
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<div style="padding: 10px 0px 10px 20px;border-top: #ccc 1px solid;background-color: #F7FBFF; text-indent:24px;">地热资源是宝贵的矿产资源,是一种可再生的,优质、环保、清洁能源。合肥是安徽省省会,经济持续快速发展对清洁地热能源的需求不断增长。据有关资料,合肥地区地处莫霍面隆起区,地壳减薄上地幔隆起是合肥地区地温相对高的大的区域地质背景。合肥西,五十里小庙凸起(合肥地区地垒地段)是基底隆起聚热型地热地质成因模式形成地热的有利地段,可作为今后合肥地区地热资源地质勘查的第一靶区。合肥地区的大地构造环境和深部地壳结构对成热条件较为有利,地热资源的潜力较大。<br>Geothermal resource is a precious mineral resource that is renewable,quality,environmentally protective and clean energy.Hefei is the capital of Anhui Province and has an ever increasing demand for clean geothermal energy to meet its economic development in a sustainable and rapid way.Based on relevant data,the Hefei area is situated at the Moho surface rise,and crustal thinning-led upper mantle lift is general regional geological setting for relative highness of earth temperature in the Hefei area.The Wushili Xiaomiao Convex in west of Hefei(the horst section of the Hefei area) is favorable to geothermal formation under the genetic model of basement uplift-caused thermal accumulation and can be the first target for geological exploration of geothermal resource in the area in the future.The tectonics and deep-seated crustal structure in the area meet the thermal formation conditions,showing great geothermal resource potential.</div>
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引文
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<div style="padding: 10px 0px 10px 20px;border-top: #ccc 1px solid;background-color: #F7FBFF; text-indent:24px;">[1]陈墨香,等.华北平原北段地热资源分布的特点[R].1982.
<br> [2]安徽省地质矿产局.安徽省区域地质志[M]合肥:安徽省科技出版社,1987.
<br> [3]王均,等.中国地温分布的基本特征[M]北京:地震出版社,1990.
<br> [4]胜利石油管理局勘探事业部.合肥盆地东北工区重力勘探解释成果报告(部分)[R].2000.
<br> [5]宁金野,等.安徽长山地热初探[J].安徽地质,2008(2).
<br> [6]王泽龙,等.北京市小汤山地区地温场特征及地下热水成因模式分析[M].北京:地质出版社,2007.
<br> [7]杨丰田,庞志和,等.苏北盆地建湖隆起区地热资源赋存特征[C]//倪四道.中国地球物理2009.合肥:中国科学技术大学出版社,2009.</div>
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