The gold mineralisation at Lamego is characterised by orebodies associated with two horizons of chemical sedimentary rocks: BIF and metachert (MCH), and also with shear zones containing abundant quartz veinlets. The proportions of these lithotypes vary substantially from one deposit to another. In the BIF, sulphide mineralisation is associated with gold, while in the MCH and quartz veins, the gold occurs either as native gold or in sulphides. Lamego shows similar rock assemblage, but with higher structural complexity than Cuiabá. The BIF which contains the mineralisation is more structurally deformed and is sometimes described as a ‘metachert’.

The mineralisation is characterised by sulphidation in the form of disseminated sulphide bands or as fracture filling and, more rarely, as massive sulphide hosted in BIF/MCH. Sulphide bands are rare in MCH. The plunge of the mineralised zones coincides with both the fold axis of the first two structural events and the mineral stretching.

The Arco da Velha deposit is located on the eastern side of a large fold and extends for 250m along the strike. In the north-eastern portion, the mineralisation is concentrated in the MCH, while in the south-western portion it is concentrated in the BIF. Carbonaceous phyllite and chlorite-sericite schists occur in the hangingwall contact, while hydrothermally-altered meta-andesite occurs in the footwall. The Cabeça de Pedra deposit is located in the hinge region of the large Lamego structure. The area which has shown the best economic potential contains BIF and MCH (80% of the area consists of BIF and the remaining 20% is MCH). The presence of faulting makes the stratigraphy complex in some areas. The carbonaceous phillite and clorite/sericite schists normally occur in the hangingwall and meta-andesites in the footwall.

CdS is located in the eastern part of the lower to middle greenschist facies archaean Rio das Velhas greenstone belt. The CdS I, II and III gold deposits and associated targets are located in a gold trend that extends for about 14km in a north-easterly direction, from Grota Funda (CdS I areas) in the south to Jambeiro (CdS III areas) in the north. The main gold targets and deposits are distributed over three trends, namely the CdS trend, the Donana Trend and the Cristina Trend. CdS mineralisation occurs in a greenstone belt geological environment, associated with quartz and sulphides (mainly arsenopyrite) in a structurally controlled corridor approximately 16 – 20km in strike length and about 500m vertical extent.

The CdS deposits consist of narrow north east/south-west elongated lenses of mineralisation dipping 60° to 70° south-east and plunging 20‚ to 30° north-east. CdS is an orogenic type deposit and comprises many hydrothermal lodes with quartz veins and low sulphide content disseminated in the wall rocks. The deposits are narrow, elongated and folded. In general, the mineralisation consists of sericitic zones and quartz veinlets.

AGA Mineração is located in southeastern Brazil in the state of Minas Gerais and encompasses mining operations at Cuiabá, Lamego, Corrego do Sitio (CdS) and The Nova Lima Sul (Raposos) project that is on care and maintenance.

The Corrego do Sitio
The Corrego do Sitio complex includes open pit and underground operations.

The underground mining method for CdS is sub-level stoping. Each panel consists of three levels with secondary development drives varying from 100m to 600m along strike. The stopes are around 15m high and the mining sequence method varies between top-down and bottom-up, which is only used in specific areas. Geotechnical parameters require that sill pillars are 4 to 7m high, and rib pillars 5m wide. The access into CdS I underground is by decline and into CdS II underground is by shaft.

The open pit operation uses conventional bench mining, with 8m individual benches and 3.2m berms. The material transport (ore and waste) is done by trucks and the excavation by a back hole. The rock breaking method varies according to the rock strength, using either explosives or mechanical excavation.

Cuiabá
Cuiabá is an underground mine, currently operates using two main mining methods: sub-level longhole open stoping, and triple stoping. A variant of sub-level longhole stoping with a free face horizontal tunnel is also applied over low inclination high-grade areas. The cut and fill mining method was reintroduced to increase ore recovery. It is applied in the narrow veins below Level 14.1 (Balancão, Galinheiro and Canta Galo orebodies) where the dip is lower. In the Galinheiro footwall, the mining method remains sub-level stoping as the orebody shows a reasonable steep dip and thickness.

Lamego
The Lamego Mine is an underground mine that operates as a satellite mine to Cuiabá Mine. All ore from mine is extracted via sub-level stopes. Ore is transported to surface via ramps where it is crushed, stockpiled and transported daily to Cuiabá Plant, where it is blended with Cuiabá ore on the ROM pad.

There are two metallurgical plants in CdS: the heap-leach plant for the oxide ore and the sulphide plant.

The sulphide process consists of crushing, grinding and gravity concentration, flotation, thickening, acidulation, pressure oxidation (POX autoclave), CCD (counter current decantation), CIL extraction, elution, neutralisation, electro-winning and tailings disposal. The plant and POX circuit have a capacity as of 600ktpy.

The heap-leaching process consist of crushing, agglomeration, stacking, leaching, adsorption, elution and electro-winning.

Cuiabá and Lamego mines feed the Cuiabá gold plant (flotation) and Queiroz (roaster, carbon circuit and refinery) plants, currently at 1.7Mtpa for a metallurgical recovery of 93.3%. At the Cuiabá gold plant, crushing and milling of the ore is followed by flotation and filtration in order to produce a concentrate, which is transported by aerial ropeway to Queiroz for further treatment. Approximately 25% to 30% ........