Cabrera-Pérez Iván, D'Auria Luca, Soubestre Jean, Del Pezzo Edoardo, Prudencio Janire, Ibáñez Jesús M, Jiménez-Mejías María, Padilla Germán D, Barrancos José, Pérez Nemesio M
Instituto Volcanológico de Canarias (INVOLCAN), Granadilla de Abona, 38600, Spain.
Department of Earth Sciences, University of Geneva, Geneva, Switzerland.
Sci Rep. 2024 Nov 9;14(1):27354. doi: 10.1038/s41598-024-79076-w.
The potential of the island of La Palma (Canary Islands) to host geothermal resources is very high, mainly due to its high volcanic activity. The primary goal of this study is to get a tridimensional image of the seismic intrinsic attenuation using ambient seismic noise and to identify anomalies that may be linked to active geothermal reservoirs on La Palma island. For this purpose, we developed a new Ambient Noise Attenuation Tomography (ANAT) technique, which uses seismic ambient noise for imaging intrinsic attenuation in 3-D at a local scale down to 5 km depth. Our research identifies two areas with high attenuation in the island's southern region. One area could be associated with hydrothermal alteration zones beneath the Cumbre Vieja volcanic complex. Another high-attenuation zone was observed in the island's southern part, which could be associated with extensively fractured rocks that might facilitate the circulation of heated fluids. Furthermore, we discuss the geothermal relevance of such anomalies, making a comparison with previous resistivity, S-wave velocity and density models. This study confirms that intrinsic attenuation retrieved from the coda of Rayleigh waves is more sensitive to the presence of fluids than velocity. Fluids being a key component of active geothermal reservoirs, it is reasonable to expect intrinsic attenuation anomalies in these systems. Therefore, we conclude that ANAT can be useful for geothermal exploration.
拉帕尔马岛(加那利群岛)蕴藏地热资源的潜力非常高,主要归因于其频繁的火山活动。本研究的主要目标是利用环境地震噪声获取地震固有衰减的三维图像,并识别可能与拉帕尔马岛活跃地热储层相关的异常情况。为此,我们开发了一种新的环境噪声衰减层析成像(ANAT)技术,该技术利用地震环境噪声在局部尺度上对深度达5千米的固有衰减进行三维成像。我们的研究在该岛南部地区识别出两个高衰减区域。一个区域可能与坎布雷维耶哈火山复合体下方的热液蚀变带有关。在该岛南部还观测到另一个高衰减带,这可能与广泛发育裂隙的岩石有关,这些裂隙可能有利于热流体的循环。此外,我们讨论了此类异常与地热的相关性,并与之前的电阻率、横波速度和密度模型进行了比较。本研究证实,从瑞利波尾波中获取的固有衰减对流体的存在比速度更为敏感。由于流体是活跃地热储层的关键组成部分,因此在这些系统中出现固有衰减异常是合理的。因此,我们得出结论,ANAT可用于地热勘探。