Geothermics ( IF 3.5 ) Pub Date : 2021-07-19 , DOI: 10.1016/j.geothermics.2021.102207 P. Sánchez-Pastor 1 , A. Obermann 1 , T. Reinsch 2, 3 , T. Ágústsdóttir 4 , G. Gunnarsson 5 , S. Tómasdóttir 5 , V. Hjörleifsdóttir 5 , G.P. Hersir 4 , K. Ágústsson 4 , S. Wiemer 1
The Hengill volcanic system is located in the Reykjanes Peninsula (Iceland) and hosts two large geothermal power plants: Nesjavellir and Hellisheiði. This area is the next target for the Iceland Deep Drilling Project (IDDP) to search for super-critical fluids. Here, we investigate the potential for ambient seismic noise tomography to be used as a geothermal exploration tool. The results are compared with different geophysical observables, of which resistivity modeling shows an excellent correlation with our results. We also observe a prominent seismic velocity reduction to the south of Hverahlíð, where the most powerful boreholes in the region are located.
中文翻译:
使用环境地震噪声层析成像对高温地热储层进行成像,以冰岛西南部 Hengill 地热田为例
Hengill 火山系统位于雷克雅内斯半岛(冰岛),拥有两个大型地热发电厂:Nesjavellir 和 Hellisheiði。该区域是冰岛深钻项目(IDDP)寻找超临界流体的下一个目标。在这里,我们研究了将环境地震噪声层析成像用作地热勘探工具的潜力。将结果与不同的地球物理观测值进行比较,其中电阻率模型显示出与我们的结果极好的相关性。我们还观察到 Hverahlíð 以南的地震速度显着降低,该地区最强大的钻孔位于此处。