Ambient seismic noise monitoring and imaging at the Theistareykir geothermal field (Iceland)

In autumn 2017 a network of 14 broadband seismic stations was deployed at the Theistareykir high temperature geothermal field (NE Iceland). This experiment was conducted as part of the current efforts to characterize the field's main structures, and possible short and long term stress variations due to the ongoing fluid injection and extraction...

Ambient noise seismic reflection interferometry at the Los Humeros Geothermal Field Mexico

In the past two decades, a limited but steadily growing number of papers were published on successful retrieval of P-wave reflections from ambient seismic noise. Subsurface reflection images can provide higher structural detail as compared to velocity images from tomographic inversion of surface waves extracted from ambient noise. But the...

Short and Long Term Variations in the Reykjanes Geothermal Reservoir From Seismic Noise Interferometry

The Reykjanes Geothermal System (RGS) is a high‐temperature geothermal system located on the Reykjanes peninsula, a transtensional plate‐boundary zone located on the southwestern tip of Iceland. The area is characterized by high seismicity, recent volcanism, and high‐temperature geothermal fields. We use seismic noise records from April 2014 to...

3D S-wave velocity imaging of Reykjanes Peninsula high-enthalpy geothermal fields with ambient-noise tomography

Tomographic imaging based on ambient seismic noise measurements has shown to be a powerful tool, especially in areas like Iceland, where the microseism illumination is excellent. In this paper, we produce a 3D S-wave tomographic image over the western Reykjanes Peninsula high-enthalpy geothermal fields and evaluate the reliability of the...

Systematic detection and correction of instrument-related time shifts using seismic interferometric surface waves

Timing errors are a notorious problem in seismic data acquisition and processing. A technique is presented that allows such time shifts to be detected and corrected in a systematic fashion. The methodology relies on virtual-source responses retrieved through the application of seismic interferometry (SI). In application to recordings of ambient...

Surface-Wave Tomography by Ambient Noise Seismic Interferometry to Image Volcanic and Geothermal Systems in South Iceland

Reykjanes ambient noise reflection interferometry

We present results from the application of ambient noise seismic interferometry (ANSI) to data that were recorded continuously in 2014 and 2015 at Iceland’s peninsula Reykjanes. The objective of this study is the retrieval of reflected body waves (P-waves) that provide high-resolution velocity-versus-depth as well as subsurface structural...