“…1), approximately 70 km wide and extending discontinuously for 800 to 1,000 km along the Peruvian littoral from Lima to the Ilo-Ite area (Clark et al, 1990;Hawkes et al, 2002;Injoque, 2002;Chen et al, 2010a), developed in the Cañete basin and, to the south, along the axis of the Jurassic-Cretaceous shallow-marine volcano-plutonic arc. Ore deposits and mineral occurrences in this belt assignable to the IOCG clan include Raúl-Condestable, Eliana, Monterrosas, Mina Justa, Cobrepampa, Rosa María, Licona, Valparaïso, and Santiago.…”