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Posts tagged with "mining"

Silver Smelting in Peru 2000 Years Ago

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On the shores of Lake Titicaca, in what is now Peru, silver was mined and smelted as early as around 2000 years ago - at Huajje. The site of Huajje is a 128,000-m3 mound located on the northern shores of Lake Titicaca, in the centre of the resource-rich Puno Bay. Huajje is situated in a region famous since Colonial times for the rich Laicacota silver ore mines located above the city of Puno.

Huajje, where the new excavations have taken place, was probably first a village that later grew out to become an important centre around 100 A.D. About 500 years later it was incorporated into the Tiwanaku state. The Incas expanded to the area in the 15th century followed by the Spaniards (looking for El Eldorado, and thus gold and not silver) after 1532. During this time-span silver was produced in Huajje.

Evidence of silver production—including crucibles, matte, slag, and vitrified ceramics characteristic of high temperature processing—was found in every level in the 22 m test unit from 0.30 m to 4.80 m below the modern surface.

The steps required for silver extraction include mining, beneficiation (i.e., crushing of the ore and sorting of metal-bearing mineral), optional roasting to remove sulfur via oxidation, followed by smelting, and cupellation. During smelting, silver and lead-rich ores are combined in the furnace. The lead ore acts as a collector for the silver metal, securing better separation of silver from the gangue (i.e., mineral impurities in the silver-bearing ore). Smelting produces metal, typically a silver-containing lead (bullion) containing variable amounts of metal sulfides (matte), and slag. Matte is defined as a matrix of metal sulfides with only minor amounts of silicates. Slag, by definition, has a matrix of silicates, sometimes with minor inclusions of matte or metal.

The data suggest the following pattern: the smelting of a rich silver ore conducted elsewhere (likely the site of Punanave), followed by transportation of the raw bullion to a central and well-supervised site (in this case, Huajje) for further processing. Re-melting of the raw bullion in crucibles here would result in the separation of matte that may have been mixed with the bullion, and a partial oxidation of lead metal, forming lead silicate slag in the crucible through reaction with quartz mineral. The refined bullion from this operation would then have been fit for cupellation to pure silver.

Note:
A crucible is a ceramic or metal container in which metals or other substances may be melted or subjected to very high temperatures.
Cupellation is a process used to separate noble metals such as gold or silver from base metals such as lead.
A cupel is a shallow, porous container in which gold or silver can be refined or assayed by melting with a blast of hot air, which oxidizes lead or other base metals.

Reference:
Schultze et al.
Direct evidence of 1,900 years of indigenous silver production in the Lake Titicaca Basin of Southern Peru
PNAS 2009
doi: 10.1073/pnas.0907733106



In Norwegian:




Academics

Lithium Mining in Tibet

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One of the reasons that China is “interested” in Tibet is (most probably) Lithium. Chabyer salt lake, in the Tibet Autonomous Region, at an elevation of 4,400 m is the largest lithium mine in China. I have of course a few problems with the name as it is transcribed from either Tibetan (or should I say Tibeto-Burman) or one of the Chinese languages. Another way of spelling it is “Zabuye”. This has lent its name to the mineral Zabuyelite, with the formula Li2CO3. Zabuyelite was discovered in 1987 at Zabuye/Chabyer Salt lake. It forms colourless vitreous monoclinic crystals. Such is the solubility of Lithium carbonate that it is unlikely to occur naturally anywhere except in evaporites and arid conditions. Chabyer salt lake is also known as Chabyer Caka. Caka is just the Tibetan word for salt lake, and actually there are more salt lakes than fresh water lakes in Tibet.

Chabyer Caka is a large bittern-salt lake (the main compounds of the salt are Lithiumcarbonate and Borax) in the Gangdisi Mountains (or is it the Lunggar Mountains?) in the interior of the Tibetan Plateau. The lake consists of two sub-basins, a southern and a northern one, joined by a narrow channel. The lake has a total area of 243 km2, a mean depth of 70 cm, and a maximum depth of less than 2 m. The salt content of the lake water is 360-410 g per litre. The basin originated through faulted structures. The underlying bedrock is Cretaceous-Eogene acidic igneous, mudstones and sandstones. A large area of playa is being exposed around the lake, and mirabilite (also known as Glauber's salt, a hydrous sodium sulfate mineral) is currently being deposited in the lake. The location of the calabash-shaped lake is 31° 20' N 84° 05' E, which I have tried to pin-point on my map of Tibet - 1050 km from Lhasa.

The lithium exploration began in 1982. By the end of 2004 it had reached a production capacity of 7500 tons of solid lithium carbonate per year. China may emerge as a significant producer of brine-source lithiumcarbonate around 2010. There is potential production of up to 55,000 tons per year if projects in Qinghai province and Tibet proceed.

The total amount of lithium recoverable from global reserves has been estimated at 35 million tonnes, which includes 15 million tons of the known global lithium reserve base.

Here follows an overview of lithium production from the U.S. Geological Survey, Mineral Commodity Summaries, January 2009.


Lithium salts are indeed found in evaporites and salt lakes. Subsurface brines have become the dominant raw material for lithium carbonate production worldwide because of lower production costs as compared with the mining and processing costs for hard-rock ores.

The market for lithium compounds with the largest potential for growth is batteries, especially rechargeable batteries. Non-rechargeable lithium batteries are used in calculators, cameras, computers, electronic games, watches, and other devices. Demand for rechargeable lithium batteries continues to grow for use in cordless tools, portable computers, mobile telephones, and video cameras. Future generations of electric vehicles may use lithium batteries (so-called lithium-ion batteries). Mitsubishi, which plans to release its own electric car soon, estimates that the demand for lithium will outstrip supply in less than 10 years unless new sources are found.

A misunderstanding seems to have crept into some of the articles. Chabyer Caka is certainly NOT one of the three largest salt lakes in the world. It may well be one of the three most important lithiumcarbonate-containing lakes ???.





Academics



Problematic Methane Mining in Lake Kivu

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In a post two years ago I featured methane in Lake Kivu.

Lake Kivu contains approximately 55 km3 of dissolved methane gas at a depth of 300 m. Previously, the methane concentration was assumed to be in steady state. However, recent analysis indicates that the methane concentration has increased significantly by 15 to 20% since the 1970s’ measurements. For carbon dioxide, the observed concentration increase was on the order of 10%, but was not statistically significant. The main hypothesis for this increased production of methane is a rise of the nutrient inputs caused by the fast-growing population in the catchment of Lake Kivu. Until 2004, extraction of the gas was done on a small scale, with the extracted gas being used to run boilers at a brewery. As far as large-scale exploitation of this resource is concerned, the Rwandan government is in negotiations with a number of parties to produce methane from the lake. Extraction is said to be cost effective and simple because once the gas rich water is pumped up the dissolved gases (primarily carbon dioxide, hydrogen sulphide and methane) begin to bubble out as the water pressure gets lower. This project is expected to increase Rwanda's energy generation capability by as much as 20 times and will enable Rwanda to sell electricity to neighboring African countries.

So far so well.

Extracting valuable methane from the lake's depths might, however, trigger an outburst of gas that could wash a deadly, suffocating blanket over the 2 million people who live around Kivu's shores.

A group of biochemists warns that if unregulated extraction continues unabated, it could trigger a catastrophic outgassing of carbon dioxide - another dissolved gas abundant in the lake's depths. Such a disaster occurred at Lake Nyos in Cameroon in 1986, killing 1700 people. Kivu contains 300 times more CO2 than Nyos did.

Like Nyos, Lake Kivu is permanently stratified: a deep layer of dense water laden with CO2, methane, salt and nutrients is locked away beneath a surface layer of fresh water. Methane is generated by lake-bed bacteria that feed on a stream of dead algae sinking from the surface. The CO2 enters through volcanic seeps.

The most dangerous practice is pumping waste water into the lake's shallows. If degassed water is dumped at the surface, it sinks, mixing water and salts between the lake's layers. Enough mixing would disrupt the density stratification of the lake, and could bring huge volumes of CO2-rich water to the surface. The pressure reduction would cause the CO2 to bubble out of solution.

Another question is of course “what could happen if the methane is NOT exploited?". Indeed the Government of Rwanda is working with experts to mitigate an imminent explosion of the gases trapped under the surface of Lake Kivu that could cause a serious human catastrophe. Recent reports suggest that the huge amounts of carbon dioxide and highly combustible methane gas trapped under the surface of Lake Kivu could explode soon if not exploited, leading to disastrous effects on the surrounding population. In an interview with the Rwandan newspaper The New Times, Charles Nyirahuku, the Head of Oil and Gas Unit in the Ministry of Infrastructure and Energy, confirmed that indeed the alarm is there but the Ministry is working round the clock with experts to ensure that the fears are mitigated. "Indeed much has been said about the danger and all this time we have been discussing possible mitigating measures. We carried out a comprehensive study and found out that one way to mitigate the danger is to extract the gas. For the moment that is what we are focusing on." (He may be biased of course?)

It is in any case evident that a strict set of rules and regulations has to be followed to ensure that the whole process of extraction is secure so that no explosion is triggered - and the possibility of one is completely eliminated.





Academics




New Massive Sulphide Deposit in the Harz?

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Hat tip to geoberg.de (in German)

The Harz Mountains in Germany have a long history of mining. Especially famous are the Mines of Rammelsberg near Goslar. These mines are a UNESCO World heritage site, known for continuous mineral extraction over a period of more than 1000 years until they finally closed down in 1988.

Now Harz Minerals (from Hamburg), a fully owned subsidiary of Scandinavian Highlands, has obtained an exploration licence for a large part of the Harz Mountains covering ca. 1250 km2. About 2 km west of the Rammelsberg mines (in the Gosetal) there are signs of a deposit maybe even larger than the Rammelsberg deposit and of a similar nature, so naturally enough the exploration targets are base metals, gold, silver and barite.

The Rammelsberg and Gosetal ores are massive sulphide deposits formed at the bottom of the Proto-Tethys Ocean that existed between the continents Laurussia and Gondwana in the Devonian (Devonian period = 416 - 359.2 million years ago). This ancient ocean existed from the latest Ediacaran to the Carboniferous (550-330 million years ago), and was closed when Laurussia and Gondwana collided with each other resulting in the so-called Variscan orogen, where a few microplates also got in between and consumed by the mountain building episode. The continental collision probably begun around 380 million years ago.

Image: Wikipedia

Note that the term Hercynian is widely used as a synonym for the Variscan. In Germany Hercynian, however refers to a Cretacious tectonic event (with northwest to southeast strike direction - like the thick black lines on the map below).

Massive sulphide deposits are not uncommon in the Variscan belt, and the main massive sulphide deposits are indicated on the following map from a handout about “The Gosetal Anomaly – a Rammelsberg twin?” that can be downloaded from the Scandinavian Highlands page about their Harz project.



Unfortunately there is no accepted definition of the term ‘massive sulphide’, but I would like to refer you to the description at http://www.encyclopedia.com/doc/1O112-massivesulphidedeposits.html . Common basic similarities shared are: cold aqueous fluid (commonly sea water) is drawn down through sediments or igneous rocks and its temperature is raised by an underlying heat source. This heat source is usually a relatively shallow magma chamber or a recent igneous intrusion.

In the Variscan context I take the deposits to be marine (hydrothermal) deposits (depth at formation estimated to be deeper than 400 m), and thus older than the Variscan orogen (when they were uplifted). The deposits marked on the map are all well described in various papers. Similar deposits are by the way found in the Moroccan Variscan Belt associated with intrusions emplaced 330 Ma ago.





Academics



3400 Years of Mercury Pollution

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Intensive mining of mercury (Hg) began around 1400 BC in the central Peruvian Andes.

Cinnabar (HgS or mercuric sulphide) is the primary natural source of mercury (Hg), and forms a bright red pigment (vermillion) when powdered. In the Andes vermillion was used as either a body paint or a covering on ceremonial gold objects from the first (Chavín) to the last (Inca) Andean empires.

PhD student Colin Cooke’s results from two seasons of field work in Peru have now provided the first unambiguous records of pre-industrial mercury pollution from anywhere in the world. His findings are published in the 18 May 2009 Early Edition of the Proceedings of the National Academy of Sciences (PNAS).

Cooke and his team recovered sediment cores from high elevation lakes located around Huancavelica, which is the New World’s largest mercury deposit. By measuring the amount of mercury preserved in the cores back through time, they were able to reconstruct the history of mercury mining and pollution in the region.

Mining appears to have began before the rise of any complex or highly stratified society (around 1400 BC). The mercury amounts peaked, however, at about 500 BC (the height of the Chavín culture) and again about 1450 AD (the height of the Inca culture, with Inca expansion into the central Andes). In between, by 800 AD, there was a brief renewal in cinnabar mining. Inca mining continued until 1564 AD when the Spanish crown assumed control,

During the Colonial era (1532–1900 AD), large-scale mercury mining began in earnest with the invention of mercury amalgamation in 1554 AD by Bartolomé de Medina in Mexico. For the next 350 years, mercury amalgamation became the dominant silver processing technique because it allowed for the extraction of silver from low-grade ores. Spanish efforts thus concentrated on supplying mercury to Colonial silver mines for use in amalgamation. Cinnabar ores from Huancavelica were smelted in grass-fired, clay-lined retorts, until vaporization yielded mercury gases, a portion of which was trapped in a crude condenser and cooled, yielding liquid mercury. Emissions of mercury thus occurred both during mining, as cinnabar dust, but also during cinnabar smelting, as gaseous mercury.

Frequent cave-ins and extensive mercury poisoning throughout Huancavelica’s 450-year Colonial history have made it one of the most sinister examples of human exploitation and disastrous mining environments ever documented, earning it the nickname mina de la muerte (mine of death).

Reference:
Cooke, C., P. Balcom, H. Biester, and A. Wolfe (2009).
Over three millennia of mercury pollution in the Peruvian Andes, Peru.
Proceedings of the National Academy of Sciences USA
doi:10.1073/pnas.0900517106

http://www.pnas.org/content/early/2009/05/15/0900517106.abstract
http://www.science.ualberta.ca/news.cfm?story=91226
http://research.eas.ualberta.ca/cooke/Colin_Cookes_Webpage/Research.html



Lithium Bonanza?

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When I was young I thought that if you had sand, you made a sand pit, if you had clay you made bricks, if you had gold you dug it out, if you had oil you pumped it up etc.

A quick glance at the following overview of lithium production from the U.S. Geological Survey, Mineral Commodity Summaries, January 2009 demonstrates that this is not always true.


High in the Andes, in a remote corner of Bolivia, in Salar de Uyuni, the world’s largest salt flat, lies more than half the world's reserves of lithium, but the output is zero.



Lithium salts are found in evaporites and salt lakes. Subsurface brines have become the dominant raw material for lithium carbonate production worldwide because of lower production costs as compared with the mining and processing costs for hard-rock ores. Two brine operations in Chile dominate the world market; a facility at a brine deposit in Argentina produces lithium carbonate and lithium chloride. A second brine operation is under development in Argentina.

The market for lithium compounds with the largest potential for growth is batteries, especially rechargeable batteries. Non-rechargeable lithium batteries are used in calculators, cameras, computers, electronic games, watches, and other devices. Demand for rechargeable lithium batteries continues to grow for use in cordless tools, portable computers, mobile telephones, and video cameras. Future generations of electric vehicles may use lithium batteries (so-called lithium-ion batteries). Mitsubishi, which plans to release its own electric car soon, estimates that the demand for lithium will outstrip supply in less than 10 years unless new sources are found.

Lithium is a limited resource and may one day be as important as to-days oil. Bolivia can become the Saudi Arabia of lithium, but for the time being it is waiting - hoping for even better times. At the same time geologists and economists are debating whether the lithium reserves outside of Bolivia are enough to meet the climbing global demand.

President Evo Morales is an ardent critic of the United States and has already nationalized Bolivia's oil and natural gas industries. For now his government talks of closely controlling the lithium itself and keeping foreigners at bay. The indigenous groups in the remote salt desert where the mineral lies are pushing for a share in the eventual bounty. Their grandparents lived on the salt. They arrived from the valleys in caravans of llamas, but the market forced them to leave. Now they want to return to live on the salar and to improve their living conditions.

I call it high stake gambling and hope for the Bolivian people that they do not become the losers in their president's gamble.

Rest to say that lithium plants produce sulphur dioxide which is a pollutant.

http://news.bbc.co.uk/2/hi/business/7707847.stm
http://www.nytimes.com/2009/02/03/world/americas/03lithium.html?_r=1
http://www.iht.com/articles/2009/02/02/america/lithium.4-421488.php
http://seekingalpha.com/article/118098-lithium-bonanza-in-bolivia

In Danish:
http://ing.dk/artikel/95515


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Mercury Pollution and the Mercury Geochemical Cycle

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Of the geochemical cycles I mentioned here the mercury cycle is the one with the smallest fluxes (Mercury is an extremely rare element in the Earth's crust, having an average crustal abundance by mass of only 0.08 parts per million). Nevertheless it is well worth watching carefully because of the toxicity of mercury. All mercury spills are potentially very dangerous.

Mercury (Hg), also known as quicksilver, is the only metal that is liquid at normal temperatures. The production of mercury has luckily declined since the early 1970s. This is partly due to increased recycling and partly to the concern about environmental pollution. Mercury is used in thermometers, barometers, manometers, sphygmomanometers, float valves, and other scientific apparatus, but concerns about the toxicity have led to mercury thermometers and sphygmomanometers being largely phased out in favour of alcohol-filled, digital, or thermistor-based instruments.

Small-scale gold mining is the second-worst source of mercury pollution in the world, after the burning of fossil fuels. Gold can be extracted by amalgamation. The principle of amalgamation is to extract gold from the pulverized ore by mercury. The ore dust is rubbed with mercury which amalgamates with the gold. The amalgam thus produced is an alloy of mercury and gold. Gold is then separated from the mercury either by filtering it through leather or by distillation. The process is forbidden in most countries, but ...

Mercury exists in two different forms, organic and inorganic. In water the most prevalent form of mercury is the organic form. Most fish have trace amounts of mercury. The level of mercury found in a fish is related to the level of mercury in its environment and its place in the food chain. Mercury tends to accumulate in the food chain, so large predatory fish species tend to have higher levels than non-predatory fish or species at lower levels in the food chain. Eating fish contaminated with mercury can cause serious health problems, especially for children and pregnant women, so the general advice in some parts of the world is not to eat fish every day.

Natural sources such as volcanoes are responsible for approximately half of atmospheric mercury emissions.

The human-generated half can be divided into the following estimated percentages:
* 65% from combustion, of which coal-fired power plants are the largest source
* 11% from gold production.
* (34% a lot of other different sources).

As I said mercury pollution has already spurred public health officials to advise eating less fish, but it could become a more pressing concern in a warmer world according to a paper that appears in a recent issue of the journal Oecologia.

Carbon dioxide, the main greenhouse gas, has increased nearly 40 percent since the industrial revolution and is expected to continue climbing unless power plant and other emissions are restricted or curtailed. Carbon dioxide-enriched soil may contain much more mercury, because such soil has greater capacity to trap and hold on to mercury.

While I was writing the first paragraphs of this post, Andrew Alden published an interesting post on mercury (12 January 2009) titled And Now, Conflict Mercury at geology.about.com.


http://www.sciencedaily.com/releases/2009/01/090107134635.htm
http://geology.about.com/b/2009/01/12/and-now-conflict-mercury.htm
http://www.msnbc.msn.com/id/28596948/
http://geology.about.com/od/mercury/a/Hgmercury.htm




PS of 15 January 2009:
The Swedish Government has forbidden all use of mercury - also in dental fillings - as from 1 June 2009.

Bauxite, Aluminium, Guinea

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Guinea is in the news just now because of the military coup after the death of the country's dictator for the last 24 years, Lansana Conté. I am interested because I am a West Africa fan. West Africa has a Gold Coast (Ghana) and an ivory Coast (Côte d'Ivoire). Guinea would deserve the name of the Bauxite Coast. Guinea could possibly have been the richest country (or at least one of the richest countries) in Africa based on the export of bauxite and other commodities if it had known a better leadership.


Guinea has the world's largest bauxite reserves (a third of the world's bauxite reserves) and is one of the biggest exporter of bauxite ore. Bauxite is the ore from which aluminium is produced. It is refined to produce alumina (aluminium oxide, Al2O3), which is further processed (by electrolysis) to make aluminium (Al). As the electrolysis demands an extremely lot of energy aluminum melting plants are often located in countries where electricity is cheap (e.g. due to hydroelectric plants). I have for instance seen a melting plant near Reykjavik in Iceland (in operation since 1969).

Aluminium is the most abundant metal in the Earth's crust, and the third most abundant element therein, after oxygen and silicon. It makes up about 8.3% by weight of the Earth’s solid surface. It is however extremely rarely found in native metal form. it was in fact once considered a precious metal more valuable than gold, because it was so hard to get at. You can become extremely rich if you can find an economic way to extract aluminium from normal clay (if such a thing as normal clay exist). Aluminium is (together with silica) abundant in all igneous rocks (like granite or basalt), mainly found in their feldspar minerals - feldspars are aluminum silicates or aluminosilicates. Aluminosilicates are also a major component of clay minerals.

Bauxite is named after Les Baux in southern France where it was discovered in 1821 by the geologist Pierre Berthier. Today Les Baux is very touristic. It is set atop a rocky limestone outcrop crowned with a ruined castle overlooking the plains to the south. Its name refers to its site - in Provençal a baou is a rocky spur.

Bauxite is a weathering product. After chemical weathering (e.g. of igneous rocks) aluminium can be concentrated in the silicate mineral, kaolinite (Al2Si2O5(OH)4). Rocks that are rich in kaolinite are known as china clay or kaolin. In tropical climate the greater availability of water (particularly in the rainy season) enables chemical weathering to progress further, so that silica is leached from kaolinite and aluminium hydroxide is left in the residue. The final weathering product may be a mixture of aluminium oxides and hydroxides of average composition Al2O3•2H2O - namely bauxite. What metals will be transported away in solution, and what metals will be left in the residue is of course a question of their solubility in ground water. Two properties of aqueous environments are here of overriding importance, namely acidity (pH) and oxidation potential (Eh).

For those who are interested I have drawn an approximate Eh-pH diagram, showing the conditions required for transport of iron and silicon and deposition of aluminium - and thereby for formation of bauxite. Oxidising solutions have values of Eh greater than 0.4 volts - a condition met in waters very close to the surface. Lower values mean a reducing potential. The main conclusion is that bauxite is formed under reducing conditions.

We may distinguish between lateritic bauxites (silicate bauxites) - as described above - and karst bauxites (carbonate bauxites). The early discovered carbonate bauxites occur predominantly in Europe and Jamaica above carbonate rocks (limestone and dolomite), where they were formed by weathering and residual accumulation of clays in limestone. I have seen such deposits in Greece, where they are still mined.

Jamaica is still a principal source of bauxite. The presence of aluminium in the red soil of Jamaica was recognised as early as 1869. Consequently there is a lot of literature about the Jamaican bauxite. In 2007, Australia was the top producer of bauxite with almost one-third world share, followed by China, Brazil, Guinea, and Jamaica.

In Europe, aluminium enjoys high recycling rates, ranging from 41% in beverage cans to 85% in building and construction and 95 % in transportation. Since the material can be recycled indefinitely without loss of quality, and because of the high intrinsic value, there are strong natural incentives to recover and recycle aluminium products after use. Comprehensive systems for the recovery of used aluminium now exist in all major European countries. 32% percent of European aluminium demand is satisfied by recycled material. A large majority of recycled aluminium is consumed by the transport sector. The other main markets are engineering, packaging and building.

http://www.nationsencyclopedia.com/Africa/Guinea-MINING.html
http://www.mining-technology.com/projects/cbg/



PS: See also "Guinean junta warns mining sector" from BBC at http://news.bbc.co.uk/2/hi/africa/7800819.stm

China now Largest Gold Producer

China produced 276 metric tons of gold in 2007. That represented just over one-tenth of the world's supply, and pushes South Africa into second place, the first time the gold giant has lost its top ranking since 1905. China's gold reserves are relatively small (about 7% of the world total). Gold production has been concentrated in the eastern provinces of Shandong, Henan, Fujian and Liaoning. Lately, remoter western provinces such as Guizhou and Yunnan have attracted keen investment from Australia and Canada,

Driving China's output higher in 2007 was increased high-grade output by the hundreds of smaller small-scale mines responsible for much of the country's output. Most of China's gold output stays in the country where it's transformed into jewellery and manufactured items, though the country's export role is increasing.

Analysts say it is unlikely that South Africa will again become top gold miner.


http://www.marketwatch.com/news/story/china-now-worlds-largest-gold/story.aspx?guid=%7B8C528CE8-0262-485D-ACEB-2247D18282CB%7D
http://www.forbes.com/2008/01/18/china-gold-production-markets-econ-cx_jc_0118markets02.html
http://www.guardian.co.uk/feedarticle?id=7246044
http://www.chinamining.org/News/2008-01-18/1200641017d8739.html




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