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Chuquicamata Copper Mine, Chile

Key Data

Chuquicamata Copper Mine, Chile

The Chuquicamata mine is a large open pit copper mine located 1,650km north of Santiago, Chile. The mine, popularly known as Chuqui, has been operating since 1910. Despite being explored for over 90 years, the mine produced 29 million tonnes of copper by the end of 2007.

The mine is owned and operated by Codelco and forms part of the company's Codelco Norte division, which includes Radomiro Tomic (RT), found on the same mineralised system, the developing Alejandro hales mine, and the newly discovered Toki cluster of copper porphyries. The Chuquicamata site is expected to be closed by 2013.

A new underground mine will be developed in addition to the present open pit mine. The conceptual engineering for the underground Chuquicamata mine began in 2007 and was finalised in March 2009.

Underground mining at Chuquicamata

The new underground mine will begin operations in 2018. Four subterranean tunnels extending 1,500km will be constructed under the surface of the mine.

The tunnels will deepen the mine by nearly 787m by the end of production in 2060. The underground mine will be developed at an estimated cost of $2bn and will produce an estimated 120,000t/d.

"The Chuquicamata mine is a large open pit copper mine located 1,650km north of Santiago, Chile."

Sinclair Knight Merz undertook the conceptual engineering of the mine, including identification, option studying and analysis for ore excavation and handling. For ore extraction, panel caving and macro blocks were studied. Three extraction panels were identified at different depths for both options. Excavation panels identified for panel cavings were at 1,841m, 1,697m and 1,409m above sea level and 1,841m, 1,625m and 1,409m for macro blocks.

The feasibility study for the underground mine was awarded to Hatch in November 2009. Hatch will oversee the basic engineering required for the development of access works, environmental studies, handling minerals, management models, infrastructure and ventilation works.

Chuqui porphyry complex geology

The Chuquicamata mine lies on the Chuqui porphyry complex, a north-north east trending, elongated, tabular, intrusive complex that measures 14kmx1.5km. The west-dipping, steep and sub-vertical complex extends from Chuquicamata to the RT mine. It also includes the east porphyry, west porphyry, banco porphyry and fine texture porphyry.


The zone's porphyries are largely affected by potassic alteration. Composed partially of alkali feldspar polymorphs and albite replacement of plagioclase, the alteration is dominated by a more widespread biotite replacement of hornblende with highly preserved igneous texture. Granular quartz apart from quartz-K feldspar veinlets also exist along with the alteration.

A significant proportion of the mine's copper is contained in veins, veinlet filling faults and fault-related shatter areas. Orebodies of the mine are controlled by west fault system, a regional sub-vertical fault trending north-south.

"The Chuquicamata site is expected to be closed by 2013."

The fault demonstrates post-mineral displacement that separates the largely mineralised Chuqui Porphyry in the east and the barren Fortuna complex in the west. The fault, belonging to the Cenozoic period, bears an usually complex kinematic past including transverse and reverse movements. The west zone is also characterised by superposition of pyritic main-stage veins with widespread quartz-sericite.

Main-stage veins running adjacent to the west fault are concentrated along a structural zone that represents a younger, breakable and shallower environment. The main-stage veins, comprising quartz, pyrite, chalcopyrite and bornite, opened up during the dextral shear of the west fault system. When the sense of shear on the west fault system changed to sinistral, north-west enargite veins also emerged.

Mining and processing

Coldec uses conventional open pit mining methods at Chuquicamata. A conventional truck-and-shovel operation constitutes the mining activity. Large quantities of the ore are crushed within the pit. Underground conveyors transport the crushed ore to the mill bins.

An Outokumpu flash smelter is installed for smelting the concentrate. The concentrate is then passed through a converter with electric furnace. After the slag is cleaned, the concentrate passes through four Pierce Smith converters. Blister copper is then sent to six anode furnaces. The electrolytic refinery has a capacity of 855,000t per annum. Three anode casting wheels were installed and are fed by the furnaces.

The mine has been operating since 1910.
The mine will be developed at an estimated cost of $2bn.