Geothermal Resources of European Continent: A Regional Assessment

F. P. Vieira, S. Guimarães, J. L. Gomes, V. Hamza
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Abstract

A regional assessment of geothermal resources of the continental region of Europe is attempted in the present work. It is based on results of observational data on heat transfer by conduction as well as hydrothermal and magmatic processes in the upper crust and makes use of geothermal data reported at the website of IHFC and also estimates based on available information on occurrences thermal springs and volcanic events. The resource assessment has been carried out for 8109 sites distributed in 39 countries. These datasets were reevaluated and spatially gridded using kigrid interpolation to construction of regional distribution maps of geothermal resources and interpreted on the basis of available information on tectonic setting and geological characteristics. The estimates for volcanic areas are based on a modified method of magmatic heat budget (MHB). has been employed in deriving estimates of geothermal resources in areas of recent volcanic activity. According to results obtained the total resource base (RB) at 6km on depth is estimated to be 8.653.306 ± 7 GJ. The mean resource base per unit area (RBUA) is ~ 985 GJ. The prominent features in geothermal maps are the presence of localities with significantly high values of resource base greater than 2000 GJ in countries such as Russia, Italy, Iceland, and west Norway. In addition, vertical distributions of temperatures were calculated in for depths reaching down to 6 km. The results obtained indicate potential availability of high temperature resources in vast regions of the European continent.
欧洲大陆地热资源:区域评价
在本工作中,试图对欧洲大陆地区的地热资源进行区域评价。它是根据关于上地壳的传导传热以及热液和岩浆过程的观测数据的结果,利用国际水文中心网站上报告的地热数据,并根据有关温泉和火山事件发生的现有信息进行估计。对分布在39个国家的8109个场址进行了资源评估。利用基格插值对这些数据进行重新评价和空间网格化,构建地热资源区域分布图,并根据现有的构造背景和地质特征信息进行解译。火山区的估算是基于一种修正的岩浆热收支(MHB)方法。已用于估算最近火山活动地区的地热资源。根据所得结果,估计6km深度总资源量RB为8.653.306±7 GJ。单位面积平均资源量(RBUA)约为985 GJ。地温图的突出特征是,在俄罗斯、意大利、冰岛和挪威西部等国,资源基础值明显高于2000 GJ。此外,还计算了深至6 km的温度垂直分布。所获得的结果表明,在欧洲大陆的广大地区,高温资源的潜在可用性。
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