“…Minimally invasive surface‐based geophysical methods can be used to fill spatial gaps between wells by producing higher lateral resolution and lower cost data (Hubbard & Linde, 2011; Parsekian et al., 2015). Over the past 10 years, an increasing number of studies have used near surface geophysics to image the architecture of the CZ (Befus et al., 2011; Braun et al., 2009; Comas et al., 2019; Eppinger et al., 2021; Leopold et al., 2013; Novitsky et al., 2018; Olona et al., 2010; Orlando et al., 2016; Parsekian et al., 2021; Pasquet, Bodet, Longuevergne, et al., 2015; St. Clair et al., 2015; Wang et al., 2021, 2022; Yaede et al., 2015). These methods measure different geophysical parameters (e.g., electrical resistivity, seismic velocity), which are sensitive to a wide range of physical properties of the subsurface materials (e.g., porosity, density, water or clay content).…”