Masbate is considered to be an example of a low sulphidation epithermal deposit, and exploration models using this deposit type are considered appropriate for the Masbate Gold Project area.

The Masbate gold deposits that are currently being mined are centred on a 5 km to 7 km wide northwest- to southeast-oriented mineralised volcanic block which is bounded by two interpreted north-west trending fault zones, the Pinanaan Fault to the east and the Malubi–Lanang–Balete Fault to the west. Approximately 31 gold vein deposits and prospects have been identified to date in the wider district, over an area of about 24 x 4 km. The mineralizing system being exploited in the open pit operations has a strike length of about 10 km, from Balete in the south to Pajo in the north. Mineralization has been tested to about 300 m depth, and remains open at depth.

The principal host rock to the gold mineralisation is a fractured andesitic–dacitic, tuffaceous agglomerate. Mineralisation occurs within quartz veins within the agglomerate, and also within associated altered and quartz stockworked wall rocks and breccias. The primary mineral associated with gold (+silver) mineralisation is quartz, both in the form of fracture-filling quartz veins and in the silicification of the host rocks. Gold is typically hosted in grey to white crystalline to chalcedonic quartz, which can sometimes be manganiferous, and is frequently associated with pyrite, marcasite, and minor amounts of chalcopyrite and sphalerite. Veins typically show epithermal colloform–crustiform banding and hydrothermal vein–breccia textures. High grade veins are generally narrow (<1 m) but some may reach 20 m in width, while sheeted zones with stockworks can reach as much 75 m in width. Individual veins may be traced for long distances, as much as 2 km. The main gold-bearing mineral is electrum.

The mine is a conventional open pit operation. Mining activities are expected to end in 2023 while stockpile processing is expected to continue until 2029. The open pit mining sequence involves grade control drilling; drill and blast operations; and excavation and hauling of materials to the process plant ROM pad, temporary LG ore stockpiles or WRSF (waste rock storage facility ).

An average of 34 Mtpa of ore and waste will be mined from five different open pits. Production in 2019 was primarily from the Main Vein pit. The primary ore source in 2020 will be the Main Vein pit, complemented by the Montana pit.

The mining and support equipment fleet was expanded in 2017 and is currently capable of annual total movement of 35 Mtpa, to meet the rate proposed in the LoM plan.

The process plant is a conventional CIL type facility consisting of primary crushing, two-stage SAG/ball mill grinding with pebble crushing, leaching, carbon adsorption; elution, electrowinning and smelting gold recovery stages; and a cyanide detoxification stage treating process plant tails before disposal in a TSF. Material is ground to 150 µm, and the leach residence time is 27 hours at the 8.0 Mtpa throughput rate.

Materials handling within the plant consists of 13 conveyor belts that are used to transport ore from the primary and supplementary crushing plants to the grinding and classification area. A 2.1 km long, 630 mm operative diameter high-density polyethylene tailings line runs from the process plant to the TSF (tailings storage facility).

The plant underwent an upgrade to 8.0 Mtpa in 2019. Currently, using the hardest ore types, the plant can treat 8.0 Mtpa consistently for the LoM. This expansion primarily consisted of adding a third ball mill and upg ........