Córdoba Fault
Geological fault in Argentina
From Wikipedia, the free encyclopedia
Córdoba Fault (Spanish: Falla de Córdoba) is a geological fault in central Argentina.[1][2] The fault is dextral and makes up the boundary between the rocks of the Pampean Orogen and Río de la Plata Craton.[1] It is considered by scientists an extension of the Trans Brazilian Lineament.[1]