“…The geometry of the tensile cracks found through MTI is superimposed onto the relocated structure, revealing en echelon fractures within Turrialba's edifice. In combination with results from previous studies [Eyre et al, 2015;Thun et al, 2015], we suggest that this structure could be a response to the deformation of the shallow part of the edifice [Bean et al, 2014], with a shearing band together with high fluid pressure inducing tensile fractures at The obtained relocation structure, when combined with the source mechanisms obtained through MTI, reveals a detailed geometrical relationship between LP sources, which can be interpreted with respect to a new, recently proposed brittle deformation-based LP source model. This study therefore highlights the need for further LP event studies to implement a more systematic relocation procedure, together with joint interpretation of the source mechanisms, to better infer the source processes of LP events within volcanoes.…”