Late Paleoproterozoic (geon 18 and 17) reactivation of the Neoarchean Great Lakes Tectonic Zone, northern Michigan, USA: Evidence from kinematic analysis, thermobarometry and 40Ar/39Ar geochronology

Polyorogenic reworking of ore‐controlling shear zones at the South Range of the Sudbury impact structure: A telltale story from in situ U–Pb titanite geochronology

“…The latter is the easternmost continuation of an Archaean suture zone, the Great Lakes Tectonic Zone, that reactivated during the Yavapai‐interval accretionary event at ca. 1.76 Ga (Riller, Schwerdtner, Halls, & Card, ; Sims, Card, Morey, & Peterman, ; Tohver, Holm, van der Pluijm, Essene, & Cambray, ).…”