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Lithological composition in deep geothermal source reservoirs of temperature 160 ?°C in the territory of Slovakia

机译:斯洛伐克境内温度为160°C的深层地热源储层中的岩性成分

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Our contribution presents the geological analysis results of the lithological composition for deep geothermal sources characterized by the thermal conditions suitable for application of classic hydrothermal sources exploitation and specialized EGS technologies for the electricity production in the territory of Slovakia. The results are presented in the form of lithological characterization for the isothermal surface depths with the reservoir temperature of 160 ?°C. The lithological conditions of geothermal source regions were constructed using available published and archive materials. From the point of view of technically utilized depths (up to 5000 m) there are two most perspective regions a?? Eastern Slovakia and Danube Basin with surrounding areas. We tried to characterize supposed lithological composition also in second category of geothermal sources between 5and 6km.
机译:我们的贡献提供了深部地热源岩性成分的地质分析结果,其特征在于适合于应用经典水热源开采的热条件和适用于斯洛伐克境内电力生产的EGS专业技术。结果以储集层温度为160°C时等温表面深度的岩性表征形式呈现。地热源区的岩性条件是使用可用的已出版和归档的材料构建的。从技术上使用的深度(最大5000 m)的角度来看,有两个最大的透视区域a?斯洛伐克东部和多瑙河盆地及周边地区。我们还试图在5至6公里之间的第二类地热源中表征假定的岩性成分。

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