Batu Hijau Gold Mine
Batu Hijau Gold Mine |
Location: Sumbawa, West Nusa Tenggara, Indonesia.
Products: Copper
& Gold.
Owner: P.T.
Newmont Nusa Tenggara.
Ore Type: Porphory Copper deposits.
Reserves: the Batu Hijau included 2.77 million tonnes of copper with an average grade of 0.69g/t gold, which would allow mining to continue until 2025.
Ore geology and Mineralization: The Batu Hijau
porphyry Cu‐Au deposit is a world‐class island arc type porphyry deposit,
located on the southwestern portion of Sumbawa Island, Nusa Tenggara Barat
Province, Indonesia. This 12 km by 6 km district contains an estimated 914
million tonnes of ore at an average grade of 0.53% Cu and 0.40 g/t Au (Garwin,
2002; Arif and Baker, 2004), and is one of the largest and richest porphyry Cu‐Au
deposits in Asia.
Ore fluids produced
distinct quartz ± sulfide veins and veinlets that cross cut the tonalite
intrusions and their surrounding host rocks. Within these veins, fluid inclusions
trapped in quartz contain ore fluids, which represent fluids moving through the
deposit during the time of its formation. The ore fluids in the fluid inclusions
are key to defining the temperature and pressure conditions under which the
deposit formed, and defining the geochemistry of the hydrothermal system, which
was responsible for the distribution Cu and Au within the deposit.
Preliminary fluid
inclusion studies have suggested that deposit formation temperatures ranged
from 280 to over 700 °C. Based on the coexistence of magnetite‐bornite ,chalcocite,
Garwin (2000) suggested that the earliest veins at Batu Hijau likely formed at
> 500–700 °C (cf. Simon et al., 2000). A preliminary fluid inclusion study
by Garwin (2000) on inclusions in halite‐bearing transitional veins produced
homogenization temperatures that ranged from about 450 to 500 °C. These
temperatures are consistent with phase equilibria temperature estimates based on a chalcopyrite , bornite
vein mineralogy (Simon et al., 2000).
Homogenization
temperatures of < 400 °C were obtained by Garwin (2000) for late pyrite‐bearing
veins. A fluid inclusion study conducted by Imai and Ohno (2005) documented
homogenization temperatures ranging from 280 to 454 °C, significantly lower
than temperatures obtained by Garwin (2000). This temperature is similar to Au
saturation temperatures for bornite (~300 °C) and chalcopyrite (250 °C) (Kesler
et al., 2002; Arif & Baker, 2004).
A detailed fluid
inclusion microthermometry study to clarify processes of ore formation is
warranted. Microthermometric data on well‐characterized fluid inclusions with
appropriate pressure corrections can provide the temperatures and pressures at
which the deposit formed. Additional qualitative and quantitative data from
synchrotron x‐ray fluorescence (SXRF) and laser ablation inductively coupled plasma
mass spectrometry (LA‐ICP‐MS), respectively, can document and quantify major
and trace element concentrations. Such data will contribute to a model describing
the transport of metals by hydrothermal fluids, and the precipitation of Cu‐
and Au‐bearing minerals.
Mining & Milling: Batu Hijau is an
open-pit mine. Ore is removed from the mining face using P&H 4100 electric
shovels (pictured) and loaded into Caterpillar 793C haul trucks. Each haul
truck can move a payload 220 t (240 short tons) of ore. The trucks haul ore
from the shovel to primary crushers. Crushed ore is sent by a conveyor 1.8 m (6
ft) wide and 6.8 km (4.2 mi) long to the mill. Daily production from the mine
is an average of 600,000 t (660,000 short tons) ore and waste combined. Ore
from the mine has an average copper grade of 0.49% and an average gold grade of
0.39g/t.
Crushed ore is further
reduced in size by Semi-Autogenous Grinding and ball mills. Once milled it is
sent through a flotation circuit which produces a concentrate with a grade of
32% copper and 19.9g/t gold. The mill realizes a copper recovery of 89%.[3] The
concentrate is thickened into slurry and piped 17.6 km (10.9 mi) to the port at
Benete where water is removed from the slurry. The concentrate storage at the
port can hold 80,000 t (88,000 short tons) of copper-gold concentrate.
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