“…For example, the buildup and release of elastic energy at geological fault is what causes earthquakes, and the intricate details of the slip zone, the propagation of slip fronts and waves radiated through the various geological media are still active areas of research (Kammer et al, 2012(Kammer et al, , 2014Roch et al, 2022). Similarly, understanding fracture in heterogeneous materials such as concrete, masonry or ceramics necessitates the modeling of interaction of crack fronts with complex materials (A. I. Cuba Ramos et al, 2018;Taheri Mousavi et al, 2015;Yilmaz et al, 2017), the representation of residual shear stresses in the contact of newly-formed crack surfaces (Pundir & Anciaux, 2021;Zhang et al, 2017), and the accurate characterization of transient dynamics (Corrado & Molinari, 2016;Vocialta et al, 2018) and material structure evolution (A. I. Cuba Ramos et al, 2018;Gallyamov et al, 2020).…”