segunda-feira, 7 de abril de 2008

THE TYPES OF DIAMOND DEPOSITS / ALLUVIAL

Angola is the third largest producer of diamonds in Africa and has only explored 40% of the diamond-rich territory within the country, but has had difficulty in attracting foreign investment because of corruption, human rights violations, and diamond smuggling.Production rose by 30% in 2006 and Endiama, the national diamond company of Angola, expects production to increase by 8% in 2007 to 10 million carats annually. The government is trying to attract foreign companies to the provinces of Bié, Malanje and Uíge. Angola has also historically been a major producer of iron ore.
1 Diamonds
2 Iron ore
3 Other minerals
4 References
Diamond mining began in 1912, when the first gems were discovered in a stream in the Lunda region in the northeast. In 1917 Diamang was granted the concession for diamond mining and prospecting, which it held until independence. Control over the company was obtained by the government in 1977. In April 1979, a general law on mining activities (Law 5/79) was enacted and gave the state the exclusive right to prospect for and exploit minerals. Accordingly, a state diamond-mining enterprise, the National Diamond Company (Emprêsa Nacional de Diamantes--Endiama), was founded in 1981 and acquired the government's 77 percent share in Diamang. UNITA, which selected the diamond mining industry as a principal target, soon crippled mining efforts, and by the beginning of 1986 the two foreign companies involved in servicing and operating the industry pulled out of Angola. By mid-1986 Diamang was formally dissolved, leaving large outstanding debts.
Attacks by UNITA on mining centers, disruption of transport routes, and widespread theft and smuggling caused diamond sales to fall to US$33 million by 1985 and to an estimated US$15 million in 1986. In late 1986, Roan Selection Trust (RST) International, a subsidiary of the Luxembourg-registered holding company ITM International, began mining in the Cafunfo area, along the Cuango River, the site of Angola's most valuable alluvial diamond deposits (see fig. 9). Mining had been halted there for more than two years after UNITA attacked the mining camp in February 1984, kidnapping seventy-seven expatriate workers and severely damaging the mining equipment. After the subsequent kidnapping of a British expatriate in November 1986, defense forces in the area were strengthened, allowing the resumption of mining operations. In 1987 production there averaged 60,000 carats, and about 120,000 carats were produced in the other two mining areas, Andrada and Lucapa. By 1987 diamond production had risen to 750,000 carats, compared with less than 400,000 carats produced in 1986. The 1987 figure, however, was still not much more than 1985 production and only a little over half of 1980 output (see table 9, Appendix A).[3]
This increase in production has benefited from the rise in the price per carat received for Angolan diamonds. The resumption of mining in the area along the Cuango River and a decline in theft of stones of higher value in the Andrada and Lucapa areas have increased the value of output. Furthermore, Endiama, which was responsible for overseeing the industry and for holding monthly sales, has benefited from a general improvement in the world diamond market as well as dealers' willingness to pay higher prices in the hope of securing favored treatment in the future. As a result, average carat value established by the monthly sales in 1987 exceeded US$110, more than twice as much as in 1985 (US$45) and at its highest level since 1981 (US$119).

In 1987 Endiama signed a two-year mining contract with the Portuguese Enterprises Corporation (Sociedade Portuguêsa de Empreendimentos--SPE), a Portuguese company that has retained a large number of Portuguese technicians previously employed by Diamang. Former Diamang shareholders founded SPE in 1979 after Diamang was nationalized. The precise terms of the contract were not made public, but it was thought that the company would undertake new prospecting, which had been at a virtual standstill since independence. Through a subsidiary, the SPE also was to help Endiama with diamond valuation, which a British company had been carrying out. In December 1987, Angola also signed an agreement with the Soviet Union to cooperate in mining diamonds and quartz. Under the terms of the agreement, the Soviet Union was to participate in mining enterprises and was to draw up a detailed geological map of Angola. In 1987 the government also began to revise the 1979 mining law to encourage new companies to invest in the diamond-mining industry, in particular to resume prospecting. Among the companies believed to be considering investing in 1988 was Britain's Lonrho conglomerate, which had taken an increasingly active interest in Angola in the late 1980s. The South African diamond-mining giant DeBeers was also interested after it lost its exclusive marketing rights for Angolan diamonds at the end of 1985 because of government suspicions that DeBeers had devalued Angolan diamonds. DeBeers has expressed interest in studying the kimberlite pipes (deep, subsurface deposits), which, because of the depletion of the alluvial deposits, were thought to represent the future of the Angolan diamond industry.
Angola is the third largest producer of diamonds in Africa and has only explored 40% of the diamond-rich territory within the country, but has had difficulty in attracting foreign investment because of corruption, human rights violations, and diamond smuggling. Production rose by 30% in 2006 and Endiama, the national diamond company of Angola, expects production to increase by 8% in 2007 to 10 million carats annually. The government is trying to attract foreign companies to the provinces of Bié, Malanje and Uíge

The Angolan government loses $375 million annually from diamond smuggling. In 2003 the government began Operation Brilliant, an anti-smuggling investigation that arrested and deported 250,000 smugglers between 2003 and 2006. Rafael Marques, a journalist and human rights activist, described the diamond industry in his 2006 Angola's Deadly Diamonds report as plagued by "murders, beatings, arbitrary detentions and other human rights violations." Marques called on foreign countries to boycott Angola's "conflict diamonds."

Iron ore
Once one of the country's major exports, iron ore was no longer mined in the late 1980s because of security and transportation problems. From the mid-1950s until 1975, iron ore was mined in Malanje, Bié, Huambo, and Huíla provinces, and production reached an average of 5.7 million tons per year between 1970 and 1974. Most of the iron ore was shipped to Japan, West Germany, and Britain and earned almost US$50 million a year in export revenue. After independence, the government established a state company, the National Iron Ore Company of Angola (Emprêsa Nacional de Ferro de Angola--Ferrangol), for the exploration, mining, processing, and marketing of iron ore. Ferrangol contracted with Austromineral, an Austrian company, to repair facilities and organize production in Cassinga. Production began to slow in 1974 as a result of technical problems at the Cassinga mine in Huíla Province and stopped completely in August 1975. The area fell under foreign control after South African forces invaded in 1975. Although South Africa withdrew its troops in early 1976, as of 1988 mining had not resumed in the area.

By 1988 the Cassinga mines had a production capacity of approximately 1.1 million tons per year. However, the railroad to the port of Namibe (formerly Moçâmedes) needed extensive repair, and since it was located only 310 kilometers north of the Namibian border, security against South African attacks could not be ensured. Furthermore, UNITA was active in the area and posed a threat to the rail line if it were repaired. Even if these problems could be resolved, production of iron ore at Cassinga would be costly in view of the depressed state of the world steel market in the late 1980s

Other minerals
In addition to diamonds and iron ore, Angola is also rich in several other mineral resources that had not been fully exploited by the late 1980s. These include manganese, copper, gold, phosphates, granite, marble, uranium, quartz, lead, zinc, wolfram, tin, fluorite, sulfur, feldspar, kaolin, mica, asphalt, gypsum, and talc. The government hoped to resume mining in the southwest for crystalline quartz and ornamental marble. It has been estimated that 5,000 cubic meters of marble could be extracted annually over a period of twenty years. A state-owned company mined granite and marble in Huíla and Namibe provinces and in 1983 produced 4,450 cubic meters of granite and 500 cubic meters of marble. Since then, the company has ceased production to re-equip with modern machinery. Quartz production, however, was suspended indefinitely because of the military situation in the areas close to the extraction sites in Cuanza Sul Province. The government established a company in 1980 to exploit phosphate deposits located in the northwest. There were 50 million tons of deposits in Zaire Province and about 100 million tons in Cabinda. Although studies of the deposits in both locations have been made by Bulgarian and Yugoslav companies, as of 1988 production had not started at either site
References
Angola: U.S. Must Strengthen Ties to Protect Strategic Energy and Security Interests
Council on Foreign Relations via AllAfrica
Angola wants foreign investors for diamond sector
July 26, 2007. Reuters Clark, Nancy. "Diamonds". Angola country study
Library of Congress Federal Research Division (February 1989). This article incorporates text from this source, which is in the public domain.
Angola to double diamond production in 2006
Afrol News , Clark, Nancy. "Iron Ore". Angola country study
Library of Congress Federal Research Division (February 1989). This article incorporates text from this source, which is in the public domain.
Clark, Nancy. "Other Minerals". Angola country study
Library of Congress Federal Research Division (February 1989). This article incorporates text from this source, which is in the public domain.
Geologic Processes
Geologic processes create two basic types of diamond deposits, referred to as primary and secondary sources. Primary sources are the kimberlite and lamproite pipes that raise diamonds from Earth's mantle, where they originate. Secondary sources, created by erosion, include such deposits as surface scatterings around a pipe, concentrations in river channels, and fluxes from rivers moved by wave action along ocean coasts, past and present. Mining of these deposits depends upon sufficient concentration and quality of diamonds.
The primary deposits, or diamond pipes, are the vertical portion. The flared top of the pipes can yield substantial quantities of diamonds, but following the narrowing pipe downward eventually becomes unprofitable. Note how erosion of the landscape moves surface minerals -- including the diamonds -- from the pipes down hills, streams, and rivers to their ultimate destination, the ocean. Because diamonds are dense they concentrate at the bottom of active zones of moving sand and gravel. These secondary deposits are eluvial &#eth; above a pipe, colluvial -- adjacent to a pipe, alluvial &#eth; stream and river transported, and marine -- along beaches that can wind up onshore or offshore with changing sea level. Secondary deposits may be found far from active means of transport, in the fossilized channels of now-vanished rivers or under fossil beaches.
Most of the diamond deposits first discovered were alluvial concentrations in streambed or riverbed sand and gravel. They are still actively exploited in many ways, from the most primitive to the highly sophisticated. The goal is relatively simple: to find a location where moving water has deposited diamonds in the bottom of a channel, possibly in a pocket or cleft. Because rivers meander and drainage can change, fossilizing a once active river, the search for alluvial diamonds requires some geological knowledge and a lot of luck. The process involves removing the overlying barren ground, digging up the bearing ground, extracting the diamonds, and, nowadays, restoring the landscape when finished.
An "independent" operation using the simplest technology: shovel, pan, water, and muscles. In the most basic, individual operations, such as in Sierra Leone or Angola, the technology involves shovel and pan, with some hand sloshing to gravitate diamond to the bottom of the pan; the eye is the ultimate sorting device. Mom-and-pop operations in South Africa involve a small claim and utilize limited technology -- shovels, buckets, jury-rigged cranes powered by small vehicles, and the like -- to load a small washing pan. The concentrate is then sieved into several size ranges, and each fraction is dumped onto a picking table, where someone checks by eye for diamonds. In the bigger operations, as shown in the model, large earth-moving equipment transports the alluvium, and the processing approaches that of the primary mines -- coarse sieving, then rotary sieving in a trommel, before loading into a large washing pan. Final processing includes concentrate sieving, a picking table, and usually a grease table. Of course, no crushing is required, as nature has already released the diamonds from the pipe rock.

There are two aspects of moving diamonds from mine to dealer. The first is the fairly straightforward but important task of separating diamonds into gem-quality, near gem-quality, and industrial-grade diamonds. The second is the more intriguing aspect: the primary diamond marketing, which has been and still is largely controlled by De Beers Consolidated Mines, Ltd. through its majority control of the Central Selling Organization (CSO). The CSO sells a large percentage of mine production to diamond dealers; independent mines sell by closed bids and through private transactions.Sorting small diamonds in a Botswanan operation. click to zoom inSorting occurs at every level of the market, from the mine to the jeweler. At the mine, the sorting depends on the sophistication of the operation and the size of production, but it is always based on grouping stones of like type. Diamonds are grouped into "sizes" -- more than one carat; "smalls" -- between 1 carat and 1/10th carat; and "sand," -- less than 1/10th carat, with some leeway for market pressures. Diamonds larger than about 15 carats are handled individually. Shape groups comprise "stones," "shapes," "cleavages," "macles," and "flats," describing characteristics familiar to the market. The ultimate purpose of sorting is to estimate an asking price for the rough diamonds. Harry Oppenheimer House is a diamond-sorting facility in Kimberley, South Africa. As in an artist's atelier, color is best judged by skylight without direct sunlight, so the windows of this building face south. Remember, South Africa is in the southern hemisphere.After great swings in diamond prices, the Diamond Trading Corporation (DTC) was set up by De Beers in 1934 to handle the actual sales of diamonds. The DTC and the Diamond Producers' Association (the mine operators) form the nucleus of the Central Selling Organization. The CSO stabilizes prices in hard times and raises them in accord with inflation and demand during good times. It needs considerable wealth and stockpiles of diamonds to maintain this position, but this "single channel marketing" system has been an effective cartel. In the United States cartels are illegal, so De Beers cannot operate here. However, the company's interests are represented by a public relations office, the Diamond Information Center, and indirectly by the diamond dealers and jewelers who sell the gems.
Alluvial Mining
Today, diamonds are mined in about 25 countries, on every continent but Europe and Antarctica (AMNH, 2006). Although most diamond mining is accomplished by large companies, in many developing countries, diamonds and other minerals are extracted by small- scale miners working in the informal sector. These small-scale miners often use simple artisanal mining techniques in alluvial deposits.
The process of alluvial diamond mining involves digging and sifting through mud, sand and gravel using shovels, sieves, or even bare hands. Typically, diamonds come from geologic rock formations called Kimberlites. Kimberlite rock formations that contain diamonds are eroded over time by rivers and streams and can deposit diamonds in the sediments carried by those streams farther downstream from the original source rocks. These deposits are called alluvial diamond deposits. The locations of these alluvial diamond deposits are controlled by the surrounding topography, drainage patterns, and the location of the Kimberlites themselves. Alluvial deposits are often mined and exploited by small-scale miners using artisanal mining techniques.
Artisanal mining techniques result in working with simple tools and equipment, usually in the informal sector, and outside the legal and regulatory framework. Artisanal operations are characterized by low productivity, lack of safety measures and high environmental impact. As a result, the majority of the artisanal miners are very poor, exploit marginal deposits with minimal returns, and are exposed to harsh and often dangerous conditions (IIED, 2006).
Artisanal and small-scale mining occurs primarily in rural areas where it represents the most promising, if not the only, income opportunity available. However, the mining activities are often viewed negatively by governments, large companies, and environmentalists. The use of child labor, the potential for environmental degradation, the high incidence of prostitution in mining camps, and the associated spread of HIV/AIDS where migrant workers are involved are major concerns in the artisanal mining sector. Further, the potential use of ASM revenue to finance conflicts and insurgencies in host countires or even regional scale conflicts is a major international concern. The use of diamond mining revenue to finance conflicts has been termed “conflict diamonds” or “blood diamonds”.
References
American Museum of Natural History. 2006. The Nature of Diamonds:
Alluvial Mining
International Institute of Environment and Development. 2006. Artisanal and Small Scale

domingo, 6 de abril de 2008

MULHERES QUE MERECEM O NOSSO RESPEITO E INCENTIVO MOTIVACIONAL

MULHERES QUE MERECEM O NOSSO RESPEITO E INCENTIVO MOTIVACIONAL
Video Miss Landmine Angola 2008

http://br.youtube.com/watch?v=jDVWJAiCD_4

video de Miss Landmine Angola 2008 - video no link no fim deste texto.

http://www.miss-landmine.org/misslandmine_project.html
Miss Landmine Angola 2008 pageant in close collaboration with the Angolan government (CNIDAH) and supported by the European Union is under way: The crowning of the world's first Miss Landmine in front of a live audience and a special jury in CineTropico in Luanda, Angola on April 2nd, 2008. The winner will receive a custom-made prothesis from Norway's leading manufacturer.

Miss minas terrestres em AngolaJovens cujo corpo foi amputado lutam contra a discriminação .O Hotel Trópico, em Luanda, foi o local escolhido para o certame "Miss Sobrevivente de Minas", com 18 representantes de cada uma das províncias angolanas.
Uma iniciativa para lutar contra a discriminação das vítimas das minas, num dos países com maior quantidade destas armas.
Apesar de todos os esforços do programa de desminagem, as Nações Unidas alertam para a existência de dezenas de milhares de minas que permanecem espalhadas pelo território de Angola, considerado o país com mais campos minados de todo o continente africano. Segundo dados do último relatório sobre as minas em Angola, da Electronic Mine Information Network (uma rede de informação sobre minas), mais de dois milhões de pessoas foram afectadas por explosões de engenhos explosivos no país.


Por ano, entre 300 e 400 pessoas morrem ou perdem membros do corpo em Angola. Elsa Cristina Neto, da sub-comissão de Apoio à Reinserção Social da Comissão Nacional Intersectorial de Desminagem e Assistência Humanitária em Angola, sabe que não se podem apagar do mapa todos os engenhos enterrados por todo o país há mais de 40 anos. Mas sabe que se pode combater o estigma social a que as amputações sujeitaram estas mulheres. E lembra que esta iniciativa tem esse objectivo.

O projecto Miss Sobrevivente de Minas 2008 foi idealizado pelo artista norueguês Morten Traavik, seguindo a tradição de concursos de beleza em Angola. O concurso de beleza, Miss Sobrevivente de Minas 2008, conta com a colaboração do governo angolano, através da comissão nacional intersectorial de desminagem e assistência humanitária (CNIDAH). Financiado pela União Europeia.
"Temos que dar uma atenção especial às mulheres vítimas de minas porque a sua condição de género já é por si um problema e são elas as principais vítimas deste problema", frisou.

Este link do video Miss Landmine Angola 2008, pode e deve ser reenviado, para todos os seus amigos, pois só tem efeitos desejáveis. Pode ajudar o MUNDO,
a ganhar consciencia deste drama, que é uma tragédia. Faça isso por AMOR.
Clique no link abaixo para visionar o video Miss Landmine Angola 2008

http://br.youtube.com/watch?v=jDVWJAiCD_4

Angola tem um concurso de miss só para vítimas das minas terrestres 'plantadas' durante a guerra civil que assolou o país. O Miss Mina Terrestre quer mostrar, segundo os organizadores, que ainda há esperança para quem perdeu a perna. De acordo com a ONU, 23 mil angolanos ficaram mutilados por conta das minas. Estima-se que ainda há milhões de minas 'enterradas' em locais desconhecidos no país. A imagem acima é de quarta-feira (2), durante a competição na capital, Luanda. (Foto: AFP)

sexta-feira, 4 de abril de 2008

General Conversion Factors - THE NORTHERN MINNER

General Conversion Factors
===========================
1 acre (ac) = 0.4047 hectares
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1 hectare (ha) = 2.471 acres = 10000 square metres = 0.00386 square miles
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1 square mile = 640 acres = 258.99 hectares = 2.59 square kilometres
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1 square kilometre = 0.3861 square miles = 247.1 acres = 100 hectares
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1 township = 36 square miles
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1 cubic foot (cu ft) = 0.028 cubic metres
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1 centare (ca) = 1550.003 square inches = 1 square metre = 1.196 square yards
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1 millimetre = 0.039 inches
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1 centimetre = 0.394 inches
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1 metre = 39.370 inches = 1.094 yards
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1 kilometre = 0.621 miles = 3280 feet = 1000 metres
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1 inch = 2.54 centimetres
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1 foot = 0.305 metres
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1 yard = 91.44 centimetres = 0.9144 metres
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1 mile = 1609.3 metres = 1.6093 kilometres
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1 litre = 0.220 gallons = 0.880 quarts = 1000 cubic centimetres = 61.025 cubic inches
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1 ounce (troy) = 31.103 grams
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1 ounce (avdp) = 28.3495 grams
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1 kilogram (kg) = 32.151 ounces (troy) = 35.274 ounces (avdp) = 2.205 pounds
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1 metric tonne = 0.984 tons (long) = 1.102 tons (short) = 2204.622 pounds = 1000 kilograms
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1 long ton (l t) = 1.016 tonnes = 2240 pounds
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1 short ton (s t) = 0.9071 tonnes = 2000 pounds
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Ore Grade Conversion
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1 troy oz./short ton = 34.2857 grams/tonne
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1 gram/tonne 0.0292 oz./ton
==================================

Specific Gravity x 1 = g/Lg/L x 8.345404 = lb/gal
lb/gal x 0.119826 = g/mL


°F = (1.8 x °C) + 32
°C = (°F - 32) x 0.555
°Kelvin = °C + 273.

Qualidade da Legislação Ambiental Brasileira: uma Discussão a partir de sua Efetividade.

Cesár, estou te enviando, em anexo, as informações formatadas.
Obrigada.
Priscila
Seminário de Meio Ambiente
Qualidade da Legislação Ambiental Brasileira: uma Discussão a partir de sua Efetividade.
Data: 17 de Abril de 2008
Horário: 8h00 às 12h30
Local: Rua da Paisagem,220 Vila da Serra – Nova Lima/MG
As leis Ambientais Brasileiras, avançadas e bem elaboradas, no que diz respeito ao objeto proposto, apresentam muitos questionamentos acerca de sua aplicação na prática, que por fatores dos mais diversos, dificultam a sua execução. Para discutir sobre a qualidade da legislação ambiental brasileira nas diferentes esferas de mercado, o Comitê de Meio Ambiente convida você a participar do Seminário de Meio Ambiente da Amcham Belo Horizonte.
Palestrantes:
Eduardo Martins – Diretor de Monitoramento e Fiscalização Ambiental do IEF
Wagner Soares Costa – Gerente de Meio Ambiente da FIMG
Alison José Coutinho – Superintendente do Ibama em Belo Horizonte
Carlos Fernandes – Presidente Nacional da Essencis

Moderador:
Joaquim Martins – Chefe do Departamento Jurídico da FEAM
Presidente:
William freire – Presidente do Comitê de Meio Ambiente da Amcham BH.
Investimento:
Sócio:R$ 30,00
Não Sócio: R$ 60,00
Informações e inscrições:
mhtml:%7B523CC2C1-A2F6-4B4A-ABF9-9FC638EBA9E8%7Dmid://00000685/!x-usc:mailto:Rafael.moretzsohn@amchambrasil.com.br
(31)2126-9750
Realização:
Câmara Americana do Comércio
American Chamber of Commerce
Patrocínio:
Hospital dos Olhos
Alcicla
Essencis MG
CBMM
Arcelor Mittal

domingo, 30 de março de 2008

GOLD UNITS from E-GOLDPROSPECTING WEBSITE

Gold UNITS !!!

Parts Per Million (PPM): A unit of concentration often used when measuring levels of pollutants in air, water, body fluids, etc. One ppm is 1 part in 1,000,000. The common unit mg/liter is equal to ppm. Four drops of ink in a 55-gallon barrel of water would produce an "ink concentration" of 1 ppm.
Parts Per Billion (PPB): One part per billion is 1 part in 1,000,000,000. One drop of ink in one of the largest tanker trucks used to haul gasoline would represent 1 ppb.
The difference between 1 ppm and 1 ppb is important. A prestigious scientific journal recently reported the concentration of a substance as 0.5-1.5 ppm. The real value was 0.5-1.5 ppb. The difference between $1 and $1000!
UNITS
PPM = mg/L, mg/Kg, ug/mL, uL/LPPB = ug/L, ug/Kg1 ppb = 0.001 ppm1 ppm = 1000 ppb20000 ug/L = 20 mg/L0.002 mg/Kg = 2 ug/Kg
PPM = Parts Per Million PPB = Parts Per BillionMilligrams per Liter = mg/LMilligrams per Killogram = mg/KgMicrograms per Liter = ug/LMicrograms per Killigram = ug/KgMicrograms per Milliliter = ug/uLMicroliters per Liter = uL/LParts Per Trillion (PPT):

A unit of concentration used to measure vanishingly small levels of pollutants or contaminants in, for example, body fluids. One ppt is 1 part in 1,000,000,000,000. One drop of ink distributed through the water contained in a total of 4 of the 3-million-gallon reservoirs pictured would result in a final concentration of 1 ppt.

The remarkable advances in the sensitivity of modern analytical techniques make it possible to detect some substances at the ppt level whose presence would not have been detected using earlier assay methods.

Parts Per Quadrillion (PPQ): One ppq is 1 part in 1,000,000,000,000,000 or 1 in 1015. Even the most modern analytical techniques cannot measure a pollutant such as dioxin in this range. However, mathematical models based on the tiny amounts of dioxin still produced during the manufacture of paper suggest that dioxin is being released in the ppq range by paper mills in the state of Maine (U.S.)

Using another mathematical model, the concept of collective dose, the U.S. Fish and Wildlife Service estimates that these undetectable levels of dioxin in river water downstream of one mill will kill, or prevent from hatching, as many as six baby bald eagles over the next five years.

Epithermal Gold Deposits

Gold deposition of epithermal Au. Mineralizing fluids ascend from hot igneous intrusion, then mix and interact with meteoric water. Epithermal gold is deposited in the boiling zone (potential bonanza deposit). Alteration of country rocks by invading hot fluids (advanced argillic alteration). Gold can also be deposited in a hot spring environment (mineralizing fluids reach the surface and cool, depositing ore) and in a placer environment (erosion of an ore body, heavy metals redeposited in sedimentary environment).
An epithermal gold deposit is one in which the gold mineralization occurs within 1 to 2 km of surface and is deposited from hot fluids. The fluids are estimated to range in temperature from less than 100C to about 300C and, during the formation of a deposit, can appear at the surface as hot springs, similar to those found in Yellowstone National Park (in northwestern Wyoming, southern Montana and eastern Idaho). The deposits are most often formed in areas of active volcanism around the margins of continents.
Epithermal gold mineralization can be formed from two types of chemically distinct fluids -- "low sulphidation" (LS) fluids, which are reduced and have a near-neutral pH (the measure of the concentration of hydrogen ions) and "high sulphidation" (HS) fluids, which are more oxidized and acidic. LS fluids are a mixture of rainwater that has percolated into the subsurface and magmatic water (derived from a molten rock source deeper in the earth) that has risen toward the surface.
Gold is carried in solution and, for LS waters, is deposited when the water approaches the surface and boils. HS fluids are mainly derived from a magmatic source and deposit gold near the surface when the solution cools or is diluted by mixing with rainwater. The gold in solution may come either directly from the magma source or it may be leached out of the host volcanic rocks as the fluids travel through them. In both LS and HS models, fluids travel toward the surface via fractures in the rock, and mineralization often occurs within these conduits. LS fluids usually form large cavity-filling veins, or a series of finer veins, called stockworks, that host the gold. The hotter, more acidic HS fluids penetrate farther into the host rock, creating mineralization that may include veins but which is mostly scattered throughout the rock. LS deposits can also contain economic quantities of silver, and minor amounts of lead, zinc and copper, whereas HS systems often produce economic quantities of copper and some silver. Other minerals associated with LS systems are quartz (including chalcedony), carbonate, pyrite, sphalerite and galena, whereas an HS system contains quartz, alunite, pyrite and copper sulphides such as enargite.
Geochemical exploration for these deposits can result in different chemical anomalies, depending on the type of mineralization involved. LS systems tend to be higher in zinc and lead, and lower in copper, with a high silver-to-gold ratio. HS systems can be higher in arsenic and copper with a lower silver-to-gold ratio.
Many countries have epithermal gold deposits, including Japan, Indonesia, Chile and the western U.S., each of which occupies a portion of the "Rim of Fire," the area of volcanism that rings the Pacific Ocean from Southeast Asia to western South America.
Epithermal gold is also found in BM any of the world's most famous gold deposits are related to subaerial volcanic activity, these are known as epithermal gold deposits. They commonly occur in island arcs and continental arcs associated with subduction. Epithermal deposits are classified as products of hydrothermal fluids which have a specific depth range. The deposits are found near the surface and mineralization occurs at a maximum depth of 1 km but it rarely exceeds a depth of 600 m. It is also considered temperatures to range from 50-300oC under conditions of moderate pressure.
Most of the ore is found in veins. They tend to be irregular branching fissures, vesicle fillings, stockworks, breccia pipes and disseminations. The most common form of emplacement is open space fillings; these include cockscomb textures, crustifications, drusy cavities and symmetrical banding. Colloform textures are also found, these are typical of a shallow volcanic environment which indicate low temperatures and the free circulation of hydrothermal fluids. Evidence for repeated mineralization is evident; this includes re-brecciation and multistage banding.
Ore minerals are usually fine grained but have coarse grained well crystallized overgrowths of gangue minerals. The ore assemblages include sulfantimonides, gold and silver tellurides, stibnite, cinnabar, native mercury, electrum, native gold, native silver, selenides and to a lesser extent galena, sphalerite and chalcopyrite. Typical gangue minerals found are quartz, calcite, fluorite, barite and pyrite. Dolomite, hematite, chlorite, rhodonite are sometimes foundritish Columbia at the Baker mine, in the Toodoggone district, and near the Taseko River.
Many of the world's most famous gold deposits are related to subaerial volcanic activity, these are known as epithermal gold deposits. They commonly occur in island arcs and continental arcs associated with subduction. Epithermal deposits are classified as products of hydrothermal fluids which have a specific depth range.
The deposits are found near the surface and mineralization occurs at a maximum depth of 1 km but it rarely exceeds a depth of 600 m. It is also considered temperatures to range from 50-300oC under conditions of moderate pressure.
Most of the ore is found in veins. They tend to be irregular branching fissures, vesicle fillings, stockworks, breccia pipes and disseminations. The most common form of emplacement is open space fillings; these include cockscomb textures, crustifications, drusy cavities and symmetrical banding. Colloform textures are also found, these are typical of a shallow volcanic environment which indicate low temperatures and the free circulation of hydrothermal fluids. Evidence for repeated mineralization is evident; this includes re-brecciation and multistage banding.
Ore minerals are usually fine grained but have coarse grained well crystallized overgrowths of gangue minerals. The ore assemblages include sulfantimonides, gold and silver tellurides, stibnite, cinnabar, native mercury, electrum, native gold, native silver, selenides and to a lesser extent galena, sphalerite and chalcopyrite. Typical gangue minerals found are quartz, calcite, fluorite, barite and pyrite. Dolomite, hematite, chlorite, rhodonite are sometimes found.

sexta-feira, 28 de março de 2008

Deposit Models - Mesothermal Gold Veins MINERAL DEPOSIT PROFILES

Deposit Models - Mesothermal Gold Veins
MINERAL DEPOSIT PROFILES


C. H. Ash, Geological Survey, B.C. Ministry of Energy, Mines and Petroleum Resources; P.H. Reynolds, Department of Geological Sciences Dalhousie University and R.W.J. Macdonald, Mineral Deposit Research Unit, Department of Geological Sciences, The University of British Columbia
Mesothermal gold quartz vein deposits in British Columbia (eg. Bralorne-Pioneer and Cassiar) and gold placer deposits derived from such veins (eg. Atlin, Cariboo, Dease Lake and Manson Creek) are, or were hosted within or marginal to collisional suture zones where large volumes of CO2-rich fluids have been channeled. These zones represent major crustal breaks between diverse assemblages of island arcs, subduction complexes and continental margin clastic wedges. They are delineated by the presence of obducted remnants of ancient oceanic lithosphere, i.e. dismembered ophiolitic rocks.
Deposits are intimately associated with carbonate altered ultramafic rocks "listwanite" derived from oceanic lower crustal plutonic or upper mantle metamorphic protoliths. The presence of such ultramafic rocks at surface, in essence characterize the trans-crustal nature of these major fault zones. Listwanite is therefore significant in that it delineates such suture zones and, more importantly marks areas where the sutures have channeled potential mineralizing fluids.
Gold mineralization is characterized by silicification, pyritization and potassic metasomatism localized along fracture zones within broader carbonate alteration halos. Economic concentrations, due to the likelihood of vein continuity and definable reserves are most likely hosted by the more competent lithologies of the obducted oceanic lithosphere, which form relatively large tectonic blocks. The differentiated mafic plutonic oceanic crustal segment of the East Lisa Complex ("Bralorne Intrusion" or "Bralorne Diorite") hosting the Bralorne gold veins and the upper crustal volcanic rocks of the Sylvester allochthon hosting the Erickson gold veins are British Columbia examples. The Grass Valley district in the Motherlode Belt was the richest and most famous gold mining district in California, with practically all the gold recovered from lodes. As at Bralorne, the veins are hosted in a mafic plutonic-volcanic section of obducted crust, the Smartville Complex.
These veins appear to form during periods of metamorphism and partial melting due to tectonic crustal thickening in response to arc-continent collision. They are typically associated with late syn-collisional intermediate to felsic magmatism. Mineralizing hydrothermal fluids are interpreted to be derived, at least in part, from tectonically thickened, hydrated oceanic lithosphere that undergoes metamorphic dehydration and partial melting during and after faulting.
Ar39/Ar40 ages of hydrothermal vein mica from the Cache Creek and Bridge River Terrane define temporally restricted mineralizing events which closely follow a collisional episode. In contrast, published K/Ar data for deposits associated with the Slide Mountain Terrane suggest that mineralization was temporally much less restrictive and formed during a period of uplift and extension in Early Cretaceous.
The available age data suggest that either:
* There are two distinct tectonic regimes of mesothermal gold-quartz vein formation in the Cordillera, one involving a collisional event and the other produced during extension and uplift, or that
* All these vein deposits are late-syncollisional and the K-Ar systematics of mesothermal vein deposits occurring in association with oceanic lithosphere above the American continental margin have been reset by later thermal events.
Mesothermal gold quartz vein deposits are found along suture zones where affected by intense and pervasive carbonate alteration that is closely associated with late syn-collisional, structurally controlled intermediate to felsic magmatism They are potentially economic where hosted by relatively large, competent tectonic blocks of obducted oceanic crust.
P - THE SNIP AND JOHNNY MOUNTAIN GOLD MINES: EARLY JURASSIC INTRUSIVE-RELATED VEIN DEPOSITS, ISKUT RIVER AREA, NORTHWESTERN BRITISH COLUMBIA David A. Rhys, Consulting Geologist
The Snip and Johnny Mountain gold mines occur five kilometres apart on Johnny Mountain in northwestern British Columbia. The area is underlain by in a folded sequence of Upper Triassic turbiditic and volcaniclastic rocks, which host the Snip mine. The Triassic rocks are unconformably overlain by flat lying Early Jurassic volcanic rocks at the Johnny Mountain mine.
Ore at the Snip mine occurs in two southwest-dipping shear veins, the Twin zone and its splay, the 150 vein, which together contain >30 tonnes Au. The deposit comprises interlayered (i) laminated calcite and chlorite-biotite-pyrite replacement shear veins and (ii) dilatant quartz and pyrite-pyrrhotite veins. Veins were emplaced progressively during normally-directed simple shear that accompanied a period of semi-brittle deformation.
The Johnny Mountain mine (Stonehouse deposit, 3 tonnes Au production) located south of Snip, consists of a set of steep north-dipping dilatant quartz-pyrite veins with K-feldspar alteration envelopes. The veins are superimposed on flat lying Early Jurassic volcaniclastic rocks that are intruded by a series of Early Jurassic feldspar porphyry dykes. Structural relations suggest that the Stonehouse veins represent a higher level, more brittle response to the same deformational event that formed the stratigraphically deeper Snip orebodies.
The Early Jurassic Red Bluff K-feldspar megacrystic quartz diorite stock intrudes Triassic rocks 300-800 metres northeast of the Twin zone. The intrusion is affected by (i) early intense quartz-magnetite-sericite-K-feldspar-biotite (potassic) alteration associated with abundant quartz-magnetite-hematite veins and Au-Cu-Mo mineralization, overprinted by (ii) sericite-pyrite-quartz (phyllic) alteration characterised by pyrite veining. Geologic relations, including similarities in alteration and structural style, geochronology, and camp-scale mineralogic and alteration zoning, indicate that intrusion, deformation, initiation of the porphyry hydrothermal system, and formation of the structurally hosted Au and base metal deposits are closely related spatially, temporally and probably genetically.
Q - INTRUSION-RELATED AU-(AG-CU) PYRRHOTITE VEINS Dani Alldrick, British Columbia Geological Survey
Intrusion-related gold-bearing pyrrhotite veins occur as a series of parallel, tabular to cymoid veins of massive iron sulphide and/or bull quartz. These moderate tonnage, high-grade veins are emplaced in en echelon fracture sets around the periphery of subvolcanic plutons. Examples of this newly-recognized deposit-type include some of the historic gold camps of British Columbia. These deposits are attractive exploration targets because of their high profit potential (high grades), ease of mining (strong, regular, structural control), relative ease of exploration (predictable restricted geologic setting; characteristic geophysical response) and high exploration potential (deposits occur in clusters or sets of veins and also have close genetic associations with other important mineral deposit types).
Veins may be composed of (i) massive fine-grained pyrrhotite and/or pyrite, or (ii) massive bull quartz with minor calcite and minor to accessory disseminations, knots and crystal aggregates of sulphides. These two dominant vein types may occur independently or together. The two mineralization styles may grade into each other along a vein, may form parallel to each other in a compound vein, or they may occur in adjacent but separate veins within an en echelon set.
The subvolcanic setting for these deposits is transitional between the setting for porphyry copper systems and the setting for epithermal systems. Mineralization is synvolcanic and syn-intrusive and formed along the thermally "brittle-ductile transition envelope" that surrounds subvolcanic intrusions. Late magma movement generated localized shearing which opened en echelon vein sets. Circulating hydrothermal fluid precipitated gold-rich iron sulphides and gangue.
All examples of this deposit type are emplaced in volcanic arc environments in oceanic or continental margin settings. These deposits have close associations with other ore deposits that are typical of arc environments. Consequently intrusion-related Au-(Ag-Cu) pyrrhotite veins should provide new exploration targets within established arc-related porphyry and epithermal camps. Conversely, discovery of these high-grade gold veins in frontier areas should spur exploration for additional deposits of this type, and for all the associated mineral deposit types of the volcanic arc environment.
Last Updated June 13, 2003

Gold, the noblest of metals, has been used by man for more than 5000 years. Its extreme softness or malleability, and resistance to tarnish (oxidation), led to its earliest uses in art and currency. Gold is the metal of choice for jewellery, and is often used in dentistry. Gold has also been used successfully in many modern technological applications. It is used as the electrical contacts of computer chips. Minute quantities of gold (less than 3 micrograms) are vaporized to mirror lens surfaces. The intrinsic value of gold offers an attractive alternative to stocks and bonds for many investors. It remains the principle medium for setting currency values and settling international debts among the nations of the world.Minor concentrations of gold occurs in most natural substances. In seawater, for example, there is approximately 0.012 parts per billion (ppb) of gold, and in fresh water it is slightly higher at 0.02 ppb. Its average concentration in the Earth's crust or lithosphere is approximately 5 ppb, and in certain sedimentary rocks it may achieve concentrations of up to 2100 ppb or 2.1 parts per million (ppm). At these concentrations 20 or 30 tons of rock must be processed to extract a single ounce of precious gold. As a result, gold can only be mined profitably where it is highly concentrated by natural chemical and physical processes.Gold occurs in many different geologic settings and its classification into deposit types is complicated. However, two basic types of occurrences or deposits are recognized, primary and secondary. Both rely on similar chemical and physical processes to produce economic concentrations of gold ore. Primary deposits form where gold precipitates during chemical reactions between hydrothermal (hot fluids) mineralizing solutions (metal-bearing)and rocks in the Earth's crust. Secondary deposits form later during the chemical and mechanical processes of weathering and erosion, and the physical reconcentration of gold-bearing sediment into placer deposits.Hydrothermal deposits can be classified as either epigenetic (deposits that form after the formation of the surrounding rocks and other events of mineralization) or syngenitic (deposits that form the same time as surrounding rocks). In epigenetic hydrothermal deposits gold may occur as the principle metal or as a secondary mineral associated with other metals, such as iron, copper, lead and zinc. In these epigenetic hydrothermal deposits. One variety of epigenetic deposit (epithermal gold deposits) form at temperatures below 350°C by the convective circulation of fluids to depths of approximately 2 kilometres, usually near hot igneous bodies or plutons in volcanically active regions. In this type of hydrothermal occurrence gold is generally at relatively low concentrations. Hot springs are modern examples of this type of mineralization process. Mesothermal gold deposits, which form at temperatures above 350°C, occur along large breaks or faults in continental crust. The origin of these is not certain, but they form at depths of 3 to 5 kilometres below the Earth's crust, and appear to be associated with the upward migration of fluids from the Earth's mantle.Gold is often extracted as a by-product during smelting from volcanogenic massive sulphide (VMS) deposits (syngenetic hyrdothermal deposits) which are generated by the accumulation of metal-rich sediments near active volcanic centres on the seafloor. Gold is also found in porphyry copper deposits, high volume (up to 1000 million tons), low grade (0.7% Cu) deposits, formed by the circulation of fluids through the Earth's crust during the volcanic activity related to mountain building above active subduction zones. Secondary gold occurrences or placer deposits are formed by the deposition and reconcentration of gold-bearing sediments from primary gold occurrences. Placer deposits are generally classified according to their depositional environment. Marine placers occur offshore near coastlines; fluvial placers occur in river and stream valleys in the drainage basins which contain primary gold occurrences upstream. Some studies suggest that gold is not only mechanically transported in placers, but that it is also chemically transported. The unusual size and purity of nuggets in some placer deposits supports this theory for gold transportation.Why is it important to continue the search for gold and other metals? Aside from the obvious financial benefits associated with the discovery and development of mineral deposits to mining companies, there are many benefits to communities fortunate enough to be located near producing mines. Exploration and mine development are activities that create jobs. They require highly trained professionals, and skilled technical personnel that may be found in local communities. In addition to the manpower and labour requirements, mineral property and mine development activities often require additional materials and specialized technical services. These are often provided by geologic and mining engineering companies, who locate offices in local communities to participate in exploration and mine development contracts. The economic "spin-offs" to communities from these activities are often significant. Resource-based activities, including mining and exploration often serve as the base for local and regional economies.Where is the gold in Newfoundland? Despite an extensive exploration and mining history, gold exploration is a relatively new activity in Newfoundland and Labrador. While the gold-bearing base metal VMS deposits, such as at the former Buchans and Rambler mines, are well known, exploration over the last two decades has resulted in the recognition of numerous epigenetic gold deposits and prospects in the province. Important recent discoveries include the Hope Brook Mine, near Burgeo, and the Pine Cove and Nugget Pond deposits, near Baie Verte. There is also excellent potential for the discovery of marine placers in regions, such as the Baie Verte Peninsula, with an abundance of primary base metal and gold deposits. The potential for fluvial placers has not been investigated, but these may be discovered in some of the larger river basins.To summarize, recent exploration in Newfoundland and Labrador has resulted in the discovery of several new, significant gold prospects. While many of these are sub-economic, a few have been successfully developed as mines. The current economic recovery in Canada, and increases in the market price of gold have already resulted in increases in the level of prospecting and exploration in Newfoundland and Labrador, activities which may lead to the development of these gold deposits. Gold should be seriously considered as a mineral commodity of great importance to the development and economic diversification of Newfoundland and Labrador. This is the ancient alchemic symbol for gold. Innumerable experiments which were focused on transforming base metals and other materials to gold made significant contributions to the science of chemistry.Further Reading
Boyle, R. W.
1979: The geochemistry of gold and its deposits. Geological Survey of Canada, Bulletin 280, 583 pages.
Brimhall, G.
1991: The genesis of ores. Scientific American, May, p. 84-91.
Rona, P. A.
1992: Deep-sea geysers of the Atlantic. National Geographic, vol. 184, no. 3, p. 105-109.
Roberts, R. G., and Sheahan, P. A.
1988: Ore deposit models. Geoscience Canada Reprint, Series 3, 194 pages.
Swinden, H. S.
1991: Regional geology and metallogeny of Central Newfoundland. In Swinden, H. S., Evans, D. W. T., and Kean, B. F. (editors) Metallogenic framework of base and precious metal deposits, Central and Western Newfoundland (Field Trip 1), Geological Survey of Canada Open File 2156, p. 7-19.
Tuach, J.
1990: List of gold occurrences and deposits in Newfoundland. Newfoundland Department of Mines and energy, Open File 1928, 72 pages.

quinta-feira, 27 de março de 2008

Vale abre 110 vagas de formação profissional em Vitória (ES)

25/03/2008
Vale abre 110 vagas de formação profissional em Vitória (ES)

A mineradora Vale está com inscrições abertas até o dia 31 de março para a primeira turma de aprendizes do curso formação profissional, que será realizada na cidade de Vitória, no Espírito Santo. São 110 vagas, sendo 62 para jovens com ensino médio e 49 vagas para os que têm com ensino técnico. O programa visa formar mão-de-obra qualificada para atuar nas áreas operacionais da empresa. Os jovens que concluíram o ensino médio irão atuar nos setores operacionais, e os que terminaram o ensino técnico trabalharão na parte técnica. A primeira fase do programa, teórica, tem duração de três meses. Os selecionados farão curso de qualificação e estudarão em tempo integral, numa instituição parceira da Vale. Na segunda etapa, com duração de seis a 12 meses, será oferecida uma formação prática que acontecerá nas unidades da empresa e com o acompanhamento de um mentor. A bolsa-auxílio será de R$ 380, na fase teórica, e a partir de R$ 800, na prática. InscriçãoPara se candidatarem, os jovens devem ter no mínimo 18 anos e ter concluído o ensino médio ou técnico (mecânica ou eletrotécnica) entre dezembro de 1997 e dezembro de 2007. As inscrições podem ser feitas no site http://www.vale.com/, na seção "oportunidade". Após a triagem de currículos, os candidatos farão prova de português e prova específica (somente para os formados no nível técnico). Na segunda fase, eles passarão por dinâmica de grupo e, na última etapa, farão entrevista pessoal com o gestor, avaliação psicológica e exame médico. A previsão de início das aulas é junho de 2008. Nos próximos meses, a Vale abrirá seleção também em Minas Gerais, Pará, Maranhão e Rio de Janeiro, oferecendo um total de 3.500 vagas.

Vale vai contratar 62 mil até 2012

segunda-feira, 24 de março de 2008

Editorial - Agência Estado Minas desprezadas agora geram fortunas


Minas desprezadas agora geram fortunas
São Paulo - 24 de Março de 2008
Outras empresas familiares já se viram diante de ofertas milionárias e até bilionárias como parte do processo frenético de consolidação dos ativos de minério de ferro localizados na Serra Azul. Desde o ano passado, além da J. Mendes, pelo menos outras quatro pequenas mineradoras foram adquiridas por grandes grupos em negócios milionários. A London Mining puxou a fila com a compra, em maio, da Minas Itatiaiuçu - em operação desde a década de 70 e dona de depósitos de 260 milhões de toneladas de minério.O valor do negócio não foi divulgado. Em meados do ano, a MMX, do empresário Eike Batista, adquiriu a AVG Mineração, localizada no município de Igarapé, por US$ 224 milhões. Por meio da AVX Mineração, a MMX também comprou a Minerminas, por US$ 125 milhões. Na mesma época, a Companhia de Fomento Mineral (CFM) foi adquirida pela CSN pelo montante de US$ 440 milhões. "A vida inteira os mineradores daquela região lutaram muito. Nunca tiveram muita facilidade, até porque essas empresas eram limitadas em termos de logística, de acesso a mercados, e forneciam basicamente para o parque guseiro.
O excesso de minério, eles vendiam para a própria Vale", observa uma importante fonte do setor, que acompanhou de perto a operação da Usiminas com a J. Mendes. "Nesse período todo, eles também fizeram pouco investimento em pesquisa geológica. Muitos não tinham a dimensão da reserva." O fato inquestionável é que o boom mundial do minério de ferro serviu para reverter a lógica da viabilidade econômica do produto. "Quem era do setor procurava as jazidas onde o teor de minério de ferro era mais alto. E o teor ali era mais baixo. Então eles não eram muito assediados pelas mineradoras maiores." Mas, quando os grandes players perceberam a disponibilidade de reservas, teve início um verdadeiro leilão.

O presidente da London Mining, Luciano Ramos, admite que a companhia, ao focar em projetos no exterior, "perdeu o time" para aquisições na região. "A Serra Azul tem uma condição privilegiada. É um minério de boa qualidade, com uma logística pronta, disponível. Além disso, as minas estão em operação, o que evita todo o processo de obtenção de licenças ambientais", destacou. "Quando você parte para a expansão, o processo tende a ser expressivamente mais rápido.
" Atualmente, entre os poucos ativos que restam na região estão duas mineradoras localizadas na pequena Itatiaiuçu: a Minerita e a MBL, dos irmãos Dílson e Edson Fonseca da Silva. Juntas, as duas mineradoras possuiriam reservas de até 450 milhões de toneladas, conforme informações não oficiais. Contatado pelo Estado, Dílson Fonseca da Silva se recusou a dar entrevista.
Minas desprezadas agora geram fortunas
Outras empresas familiares já se viram diante de ofertas milionárias e até bilionárias como parte do processo frenético de consolidação dos ativos de minério de ferro localizados na Serra Azul. Desde o ano passado, além da J. Mendes, pelo menos outras quatro pequenas mineradoras foram adquiridas por grandes grupos em negócios milionários. A London Mining puxou a fila com a compra, em maio, da Minas Itatiaiuçu - em operação desde a década de 70 e dona de depósitos de 260 milhões de toneladas de minério.O valor do negócio não foi divulgado. Em meados do ano, a MMX, do empresário Eike Batista, adquiriu a AVG Mineração, localizada no município de Igarapé, por US$ 224 milhões. Por meio da AVX Mineração, a MMX também comprou a Minerminas, por US$ 125 milhões. Na mesma época, a Companhia de Fomento Mineral (CFM) foi adquirida pela CSN pelo montante de US$ 440 milhões. "A vida inteira os mineradores daquela região lutaram muito. Nunca tiveram muita facilidade, até porque essas empresas eram limitadas em termos de logística, de acesso a mercados, e forneciam basicamente para o parque guseiro.
O excesso de minério, eles vendiam para a própria Vale", observa uma importante fonte do setor, que acompanhou de perto a operação da Usiminas com a J. Mendes. "Nesse período todo, eles também fizeram pouco investimento em pesquisa geológica. Muitos não tinham a dimensão da reserva." O fato inquestionável é que o boom mundial do minério de ferro serviu para reverter a lógica da viabilidade econômica do produto. "Quem era do setor procurava as jazidas onde o teor de minério de ferro era mais alto. E o teor ali era mais baixo. Então eles não eram muito assediados pelas mineradoras maiores." Mas, quando os grandes players perceberam a disponibilidade de reservas, teve início um verdadeiro leilão.
O presidente da London Mining, Luciano Ramos, admite que a companhia, ao focar em projetos no exterior, "perdeu o time" para aquisições na região. "A Serra Azul tem uma condição privilegiada. É um minério de boa qualidade, com uma logística pronta, disponível. Além disso, as minas estão em operação, o que evita todo o processo de obtenção de licenças ambientais", destacou. "Quando você parte para a expansão, o processo tende a ser expressivamente mais rápido.
" Atualmente, entre os poucos ativos que restam na região estão duas mineradoras localizadas na pequena Itatiaiuçu: a Minerita e a MBL, dos irmãos Dílson e Edson Fonseca da Silva. Juntas, as duas mineradoras possuiriam reservas de até 450 milhões de toneladas, conforme informações não oficiais. Contatado pelo Estado, Dílson Fonseca da Silva se recusou a dar entrevista.

sexta-feira, 21 de março de 2008

PARABENS PELA AÇÃO - Mineração em Terras Indígenas é debatida na Câmara dos Deputados

NA FOTO
Da direita para a esquerda: Miguel Nery (DNPM), Claudio Scliar (SGM-MME), Dep. Édio Lopes (Presidente da Comissão), Dep. Eduardo Valverde (Relator), Aloysio Guapindaia (FUNAI) e Agamenon Dantas (presidente da CPRM)

Mineração em Terras Indígenas é debatida na Câmara dos Deputados
19/03/2008 - 09:50
Foi realizada dia 18/03/2008, na Câmara dos Deputados, audiência pública na Comissão Especial Sobre Exploração de Recursos Minerais em Terras Indígenas. A mesa diretora da comissão é composta pelo dep. Édio Lopes (Presidente) e Dep. Eduardo Valverde (relator) Participaram da audiência o secretário de Geologia, Mineração e Transformação Mineral do Ministério de Minas e Energia, Cláudio Scliar; o diretor-geral do DNPM, Miguel Antonio Cedraz Nery; o diretor- presidente da Companhia de Pesquisa de Recursos Minerais (CPRM), Agamenon Sérgio Lucas Dantas; o vice-presidente da Fundação Nacional do Índio (Funai), Aloysio Guapindaia.Em sua fala, o secretário de Geologia, Mineração e Transformação Mineral do Ministério de Minas e Energia, Cláudio Scliar, detalhou o projeto que será apresentado pelo Executivo ao Congresso para regular o assunto.O diretor-geral do Departamento Nacional de Produção Mineral, Miguel Nery, destacou que o País hoje conta com 5.643 processos sobrestados de requerimentos para exploração mineral em reservas indígenas. Explicou que, somente para exploração de ouro, são 2.753 pedidos. "Como as empresas realizam pesquisa de exploração, esses números dão uma idéia das riquezas que podem existir nesses territórios." Na opinião do direto-geral, é importante que a regulamentação da exploração de minérios em terras indígenas ocorra o mais rapidamente possível. Entende o diretor-geral que no processo de definição da lei, devam ser observados a autodeterminação dos povos indígenas sobre as possibilidades de desenvolvimento sustentável de suas comunidades, respeitando o modo de vida tradicional dos povos indígenas. Segundo Miguel Nery, “a mineração atual é mais respeitosa com o meio-ambiente e é socialmente aceitável. A sua atividade certamente criará consições para que haja qualificação profissional dos indígenas bem como possibilitárá a autosustentabilidade financeira daquelas comunidades. Além do mais, a mineração será fonte de emprego e renda para os povos indígenas, seus projetos de trazem consigo infraestrutura local e regional e podem elevar a qualidade de vida dessas populações que são muito carentes.A não regulamentação da mineração em terras indígenas, impede o Estado fazer a gestão dosa recursos minerais das reservas indígenas e estimula a marginalização dos índios.O diretor-presidente da Companhia de Pesquisa de Recursos Minerais, destacou a necessidade de conhecimento geológico do território brasileiro. Para Agamenon, esse conhecimento prévio poderia evitar inúmeros conflitos em terras indígenas por permitir, por exemplo, o planejamento racional dessas áreas.O vice-presidente da Fundação Nacional do Índio, afirmou que a Funai reconhece a importância da regulamentação da exploração de recursos minerais em reservas indígenas. Em sua opinião, no entanto, faz-se necessário discutir os demais aspectos relacionados a essas comunidades.

DNPM - Assessoria de Comunicação