In simplest geological terms, Argentina occupies part of the South American platform in the north, the Patagonian platform in the south and the Andes mountains in the west.
The Precambrian-Paleozoic crystalline basement of Argentina comprises plutonic intrusives (granites to gabbros) and metamorphosed sedimentary and volcanic rocks that host a range of styles of mineralization that contain a variety of metals including nickel, copper, chromium, platinum group metals, tungsten, tin, silver and gold deposits and showings.
The crystalline basement is overlain by Paleozoic to Cenozoic continental and marine sedimentary rocks that also host a range of mineral deposits and showings containing a variety of metals including lead, zinc, silver, copper, uranium and vanadium.
Volcanic-intrusive activity during late Paleozoic and Mesozoic times generated porphyry copper and high sulphidation epithermal gold-silver deposits in the Andes as well as epithermal gold-silver and polymetallic mineralization in Patagonia. Important sediment-hosted uranium deposits also formed in Patagonia in the Mesozoic.