segunda-feira, 12 de setembro de 2016

Qual é o segredo da Austrália, o país que está há 25 anos sem sofrer uma recessão

Qual é o segredo da Austrália, o país que está há 25 anos sem sofrer uma recessão

É preciso voltar muito no tempo para encontrar uma fase de crise na economia australiana. Em 1990, a seleção argentina, encabeçada por Maradona, era campeã de futebol. Os poucos telefones celulares em operação eram do tamanho de um tijolo de construção. E a União Soviética estava em seu processo final de desintegração.
Desde 1991, e por 25 anos consecutivos, a economia australiana só vem crescendo. Os dados mais recentes, de junho, mostram que a economia está crescendo a um ritmo anual de 3,3%. Só faltam três trimestres para que a Austrália alcance o recorde de maior crescimento econômico contínuo na época moderna – que atualmente pertence à Holanda: 26 anos.
Economia diversificada
O bom desempenho experimentado pela economia australiana tem ainda mais mérito devido ao colapso dos preços internacionais das matérias-primas – uma tendência ameaçadora para uma nação voltada para a mineração. A explicação pode ser encontrada, parcialmente, na boa sorte, segundo a correspondente de economia asiática da BBC, Karishma Vaswani.
“As minas foram fechadas e empregos foram perdidos nesse setor. Mas não esqueçamos que a Austrália é uma economia altamente diversificada”, afirmou.
“Turismo, finanças, tecnologia e educação são os componentes principais da economia da Austrália e se beneficiaram de uma moeda australiana mais fraca”, segundo a correspondente.
Também ocorreram lucros no setor agrícola e a mesma indústria de mineração obteve um alívio na recente desvalorização do dólar australiano, o que fez os produtos do país ficarem mais baratos no exterior.
E os avanços tecnológicos a fizeram mais competitiva.
Alto padrão de vida
Mas, independente do desenvolvimento recente, o fato é que a Austrália está há mais de uma geração sem conhecer uma verdadeira crise econômica. O país conta com abundantes recursos naturais e seu território tem dimensões continentais.
Conta com recursos minerais, mas também se beneficiou com correntes migratórias que levaram profissionais e empresários de todo o mundo para viver no país. A Austrália atrai novos habitantes, em parte com a promessa de uma boa qualidade de vida em meio a praias, natureza e um clima agradável – além de cidades cosmopolitas como Sydney e Melbourne.
O desemprego está um nível baixo, de cerca de 5%. E há muitos australianos que nunca experimentaram uma crise econômica. Mas analistas advertem que com uma demanda externa que às vezes vacila, um elevado nível de endividamento de seus habitantes e outros fatores que diminuem o consumo, não se pode descartar uma desaceleração do crescimento.
Por isso, a Austrália não pode se descuidar nos 9 meses que faltam para alcançar a Holanda e ficar com a medalha de ouro no crescimento econômico mundial.
Fonte: G1

Chinesa CBStell investe na construção de siderurgia no Brasil

Chinesa CBStell investe na construção de siderurgia no Brasil

A empresa chinesa CBStell vai investir 3,5 mil milhões de dólares na construção de uma siderurgia em Bacabeira, no estado brasileiro de Maranhão, no Brasil, com capacidade de produzir três milhões de toneladas de aço por ano, anunciou o governo brasileiro. Numa segunda fase a CBStell investirá mais 4,5 mil milhões de dólares para que a capacidade produtiva aumente para 10 milhões de toneladas de aço por ano.
O financiamento será da China Brazil Xinnenghuan International Investment Co Ltd. A empresa mineira brasileira Vale anunciou, entretanto, ter assinado um memorando de entendimento (MoU) com a CBStell com vista a uma parceria que permita à Vale receber minério de ferro da nova siderurgia.
O acordo foi firmado em Xangai durante um seminário e encontro de empresários organizado pelo governo do Brasil destinado a atrair investidores chineses para o Brasil. O projecto, que inclui a construção de um porto, irá criar cinco mil postos de trabalho no nordeste do Brasil.
Fonte: Macauhub

domingo, 11 de setembro de 2016

Types of Opal

Types of Opal



Types of Opal
Opal is a hydrated amorphous form of silica; its water content may range from 3 to 21% by weight, but is usually between 6 and 10%. Because of its amorphous character, it is classed as a mineraloid, unlike the other crystalline forms of silica, which are classed as minerals. It is deposited at a relatively low temperature and may occur in the fissures of almost any kind of rock, being most commonly found with limonite, sandstone, rhyolite, marl, and basalt.
Opal is the national gemstone of Australia. Australian opal has often been cited as accounting for 95-97% of the world’s supply of precious opal, with the state of South Australia accounting for 80% of the world’s supply. Recent data suggests that the world supply of precious opal may have changed. In 2012, Ethiopian opal production was estimated to be 14,000 kg (31,000 lb) by the United States Geological Survey. USGS data from the same period (2012), reveals that Australian opal production to be $41 million. Because of the units of measurement, it is not possible to directly compare Australian and Ethiopian opal production, but these data and others suggest that the traditional percentages given for Australian opal production may be overstated. Yet, the validity of data in the USGS report appears to conflict with that of Laurs and others and Mesfin, who estimated the 2012 Ethiopian opal output (from Wegal Tena) to be only 750 kg (1,650 lb).
The internal structure of precious opal makes it diffract light; depending on the conditions in which it formed, it can take on many colors. Precious opal ranges from clear through white, gray, red, orange, yellow, green, blue, magenta, rose, pink, slate, olive, brown, and black. Of these hues, the reds against black are the most rare, whereas white and greens are the most common. It varies in optical density from opaque to semitransparent.
Common opal, called “potch” by miners, does not show the display of color exhibited in precious opal.

Types of Opal

Black Opal

Locality: Grawin & Glengarry Opal Fields,Lightning Ridge, Finch Co.,New South Wales, Australia Dimensions: 23 mm x 10 mm x 3.8 mm Copyright © Miklos Brezanszky
Black opal is characterised by a dark body tone causing brightness of colour which is unmatched by lighter opals. Black Opals are usually mined in Lightning Ridge, New South Wales, and are the most famous, and sought-after type of opal. The term ‘black opal’ does not mean that the stone is completely black (a common mistake), it simply means the stone has a dark body tone in comparison to a white opal.
Australian black opals are the most valuable and widely known type of opal. Black opal is characterised by a dark body tone which can range from dark grey to jet black. (See the following chart). However this refers only to the general body tone of the stone, and is not related to the rainbow or spectral colours present in the opal. Some people expect a black opal to be completely black (in which case it would be completely worthless).

White Opal

11.0 x 7.0 x 2.5 mm
Also known as ‘milky opal’, white opal features light white body tones, and is mined in South Australia. White opal is more common and because of its body tone, generally does not show the colour as well as black opal. Nevertheless, white opals can still be absolutely magnificent in colour if a good quality stone is found.

Boulder Opal

Locality: Queensland, Australia Dimensions: 123 mm x 65 mm x 45 mm Copyright © Lopatkin Oleg
Boulder opal forms on ironstone boulders in Queensland. This type of opal is often cut with the ironstone left on the back, as the opal seam is usually quite thin. Leaving the ironstone on the back means that boulder opal can be very dark and beautiful in colour. The opal forms within the cavities of the boulders in both vertical and horizontal cracks. Boulders vary in shape and size, from as small as a pea, to as big as a family car. Boulder Opal has a tendency to cleave; when cleaved the “split” leaves two faces of opal, with a naturally polished face.

Crystal Opal

7.75 ct. Lightning Ridge Crystal Opal Credit: Mardon Jewelers
Crystal opal is any of the above kind of opal which has a transparent or semi-transparent body tone – i.e. you can see through the stone. Crystal opal can have a dark or light body tone, leading to the terms “black crystal opal” and “white crystal opal”.

Fire Opal

Locality: Opal Butte, Morrow Co., Oregon, USA 3 cm wide specimen Copyright © Peter Cristofono
Is a transparent to translucent opal, with warm body colors of yellow to orange to red. Although it does not usually show any play of color, occasionally a stone will exhibit bright green flashes. The most famous source of fire opals is the state of Querétaro in Mexico; these opals are commonly called Mexican fire opals. Fire opals that do not show play of color are sometimes referred to as jelly opals. Mexican opals are sometimes cut in their ryholitic host material if it is hard enough to allow cutting and polishing. This type of Mexican opal is referred to as a Cantera opal. Also, a type of opal from Mexico, referred to as Mexican water opal, is a colorless opal which exhibits either a bluish or golden internal sheen.

Girasol Opal

Is a term sometimes mistakenly and improperly used to refer to fire opals, as well as a type of transparent to semitransparent type milky quartz from Madagascar which displays an asterism, or star effect, when cut properly. However, the true girasol opal is a type of hyalite opal that exhibits a bluish glow or sheen that follows the light source around. It is not a play of color as seen in precious opal, but rather an effect from microscopic inclusions. It is also sometimes referred to as water opal, too, when it is from Mexico. The two most notable locations of this type of opal are Oregon and Mexico.

Peruvian Opal  (also called Blue Opal)

Is a semiopaque to opaque blue-green stone found in Peru, which is often cut to include the matrix in the more opaque stones. It does not display pleochroism. Blue opal also comes from Oregon in the Owhyee region, as well as from Nevada around Virgin Valley.


Natural Diamond Colors

Natural Diamond Colors

Natural Diamond Colors
Diamond is a metastable allotrope of carbon, where the carbon atoms are arranged in a variation of the face-centered cubic crystal structure called a diamond lattice. Diamond is less stable than graphite, but the conversion rate from diamond to graphite is negligible at standard conditions. Diamond is renowned as a material with superlative physical qualities, most of which originate from the strong covalent bonding between its atoms. In particular, diamond has the highest hardness and thermal conductivity of any bulk material. Those properties determine the major industrial application of diamond in cutting and polishing tools and the scientific applications in diamond knives and diamond anvil cells.
Most natural diamonds are formed at high temperature and pressure at depths of 140 to 190 kilometers (87 to 118 mi) in the Earth’s mantle. Carbon-containing minerals provide the carbon source, and the growth occurs over periods from 1 billion to 3.3 billion years (25% to 75% of the age of the Earth). Diamonds are brought close to the Earth’s surface through deep volcanic eruptions by a magma, which cools into igneous rocks known as kimberlites and lamproites. Diamonds can also be produced synthetically in a HPHT method which approximately simulates the conditions in the Earth’s mantle. An alternative, and completely different growth technique is chemical vapor deposition (CVD). Several non-diamond materials, which include cubic zirconia and silicon carbide and are often called diamond simulants, resemble diamond in appearance and many properties. Special gemological techniques have been developed to distinguish natural diamonds, synthetic diamonds, and diamond simulants
A chemically pure and structurally perfect diamond is perfectly transparent with no hue, or color. However, in reality almost no gem-sized natural diamonds are absolutely perfect. The color of a diamond may be affected by chemical impurities and/or structural defects in the crystal lattice. Depending on the hue and intensity of a diamond’s coloration, a diamond’s color can either detract from or enhance its value. For example, most white diamonds are discounted in price when more yellow hue is detectable, while intense pink or blue diamonds (such as the Hope Diamond) can be dramatically more valuable. Of all colored diamonds, red diamonds are the rarest. The Aurora Pyramid of Hope displays a spectacular array of naturally colored diamonds, including red diamonds.

Diamond Colors

Diamonds occur in a variety of colors; steel gray, white, blue, yellow, orange, red, green, pink to purple, brown, and black. Colored diamonds contain interstitial impurities or structural defects that cause the coloration, whilst pure diamonds are perfectly transparent and colorless.

Brown Diamonds

Brown diamonds are the most common color variety of natural diamonds. The brown color makes them less attractive as gemstones because of the reduced glimmer, and most are used for industrial purposes. However, improved marketing programs, especially in Australia and the United States, have resulted in brown diamonds becoming valued as gemstones in recent years and even referred to as chocolate diamonds.
A significant portion of the output of Australian diamond mines is brown stones. A large amount of scientific research has gone into understanding the origin of the brown color. Several causes have been identified, including irradiation treatment, nickel impurities and lattice defects associated with plastic deformation; the latter is considered as the predominant cause, especially in pure diamonds. A high-pressure high-temperature treatment has been developed that heals lattice defects and converts brown diamonds into yellow or even colorless stones.

Orange Diamonds

The vast majority of all diamonds contain some nitrogen. In orange diamonds the nitrogen atoms have grouped themselves in a very specific way. This happens during and right after the diamond is formed. These nitrogen arrangements absorb light in the blue and yellow region of the spectrum producing an orange color. Orange Diamonds may contain a brown, yellow or pinkish modifying color.
The majority of orange diamonds come from Africa. The interest in this color surged in 1997 with the auction of the Pumpkin Diamond, so named by the buyer Ronald Winston as it was purchased the day before Halloween. The 5.54 carat vivid orange diamond, was at the time the largest vivid orange diamond ever found.

Yellow Diamonds

Yellow diamonds the nitrogen atoms have grouped themselves in very specific ways. This happens during and right after the diamond is formed. These nitrogen arrangements absorb light in the blue region of the spectrum producing a yellow color. Yellow diamonds can contain an orange, green or brown modifying color.
The most notably large and intense yellow diamonds have been discovered primarily in South Africa. The Allnatt, a 101ct cushion shape fancy vivid yellow diamond is perhaps the most signifi cant yellow diamond in history, named after its original owner Major Allnatt in the 1950s. One of the largest polished diamonds in the world is the Incomparable, a 407ct internally flawless brownish yellow diamond.

Green Diamonds

Green diamonds acquire their color after their trip to the earths surface when they rest in the ground near naturally occurring radiation. This radiation pushes into the diamond causing absorption in the red and yellow regions of the spectrum producing a green color. Green Diamonds can contain a yellowish, bluish or grayish modifying color.
Green diamonds are found predominately in regions of Africa and South America. The Dresden Green is the most famous green diamond. Weighing approximately 41 carats, it is often referred to as the cousin of the Hope Diamond for its historical importance. predominately in regions of Africa and South America. The Dresden diamond. Weighing approximately 41 carats, it is often referred to as the cousin of the Hope Diamond.

Blue Diamonds

The bonding of boron to carbon causes absorption in the red, yellow and green parts of the spectrum producing a blue color. Blue Diamonds may contain a gray, violet or greenish modifying color.
The Cullinan mine and Golconda region are the most notable areas where blue diamonds have come from. The most famous blue diamond in history is the 45 carat Hope Diamond. In 2008 The Wittelsbach Diamond, a 35.56 carat ushion-shaped fancy deep blue, was purchased at auction for $24 million. Experts compare this stones color and characteristics to the famed Hope Diamond.

Pink Diamonds

Diamonds become pink when heat and pressure deep within the earth cause the crystal lattice to distort. These distortions cause Pink Diamonds to absorb green light and hence impart a pink color. This can often be seen as in parallel bands within the diamond. Pink Diamonds may be modifi ed by an orange, brown or purplish color.
Pink diamonds can be graded faint, very light, light, fancy light, fancy intense, fancy deep and fancy vivid. And like other hues, the stronger the color, the higher the price tag.
Pink diamonds often feature secondary hues – an additional modifying color. The most common modifying colors are orange, brown and purple.
Natural pink diamonds can be found in Brazil, Russia, Siberia, South Africa, Tanzania and Canada. However, the majority of these breathtaking stones hail from the Argyle Mine in Australia, which is owned by Rio Tinto. The firm’s headquarters is also in Perth, Western Australia.
Here, the finest quality pink diamonds from the Argyle mine are cut and polished before they are sold via an exclusive tender. For proportions and to understand the rarity of pink diamonds, out of every 1 million carats of rough diamonds that the mine produces, just 1 carat is suitable to sell.

Red Diamonds

Red diamonds are extremely rare. Basically they are very strongly and deeply colored pink diamonds, with the same cause of color, crystal distortion. This combination is so rare that most jeweler and diamond dealers have never even seen a natural red diamond. They do not get large with the 5.11 carat Moussiaf Red shield being the largest known red.

Purple Diamonds

Purple diamonds are very rare. It is believed that they have a similar cause of color as pink diamonds; crystal distortion. They are most often found in Siberia and are generally small in size. There are no historical or famous purple diamonds. This may be due to their inhospitable location. Purple diamonds larger than 5 carats are extremely rare, and their color rarely reaches the intense and vivid color grades.

Violet Diamonds

Violet diamonds are very rare. The vast majority come from the Argyle mine, the same mine that most strongly colored pink diamonds are found. Their color is related to Hydrogen, but the exact mechanism is as yet unknown. They are often very small and diamonds greater than 1 carat are extremely rare. Their color usually has a gray component, diamonds of a pure violet color represent less than 10% of all violets. The number of intense and vivid violet diamonds mined each year could be counted on one hand.

Olive Diamonds

Olive diamonds are often confused with green diamonds, but they populate a different and discrete area of color space. Their color is a combination of yellow and green sometimes also a bit of brown or gray. They often come with three colors to describe them such as brownish greenish Yellow, and while this does accurately describe the color olive is a simpler, more concise term. They can range is size from small to large (some are 10+ carats). Occasionally they exhibit a color change when heated or left in the dark, these are known as chameleon diamonds.

Black Diamonds

Natural color black diamonds are rare. Their color is due to dark inclusions within the diamond, usually made up of graphite. It is rare that they are large, but the most famous black diamond, the Black Orloff, is 67.50 carats. Usually they are opaque and much of their beauty is the bright, adamantine luster that reflects light off the surface. Often used as melee in fashion jewelry in combination with colorless diamonds black diamonds are becoming very popular.

White Diamonds

Natural color white diamonds are not colorless, but are actually white. This can often cause confusion as the term is used loosely. A pure white diamond has a translucency or even opacity that makes the diamond white. This is often caused by sub-microscopic inclusions. They occasionally exhibit a weak play of color (similar to opals) called opalescence. These are highly prized among conniseurs.

Gray Diamonds

Gray diamonds are often steely in appearance and to an untrained eye may be hard to distinguish from colorless diamonds. When viewed side-by-side the difference is obvious, a gray diamond is darker than a colorless one. Pure gray diamonds are rare and are frequently described as a masculine color diamond.

Reference:
Wikipedia: Diamond



Diamond

Diamond


7
Locality: Kimberley, Francis Baard District, Northern Cape Province, South Africa Dimensions: 7 mm x 6 mm x 6 mm “Courtesy of Rob Lavinsky, The Arkenstone, www.iRocks.com”
Chemical Formula: C
Locality: Kimberly, republic of South Africa. India. Brazil. Ural Mountains, Russia. Murfreesboro, Arkansas, USA.
Name Origin: From the Greek, adamas, meaning “invincible” or “hardest.”
In mineralogy, diamond is a metastable allotrope of carbon, where the carbon atoms are arranged in a variation of the face-centered cubic crystal structure called a diamond lattice. Diamond is less stable than graphite, but the conversion rate from diamond to graphite is negligible at standard conditions. Diamond is renowned as a material with superlative physical qualities, most of which originate from the strong covalent bonding between its atoms. In particular, diamond has the highest hardness and thermal conductivity of any bulk material. Those properties determine the major industrial application of diamond in cutting and polishing tools and the scientific applications in diamond knives and diamond anvil cells.

Natural history

The formation of natural diamond requires very specific conditions—exposure of carbon-bearing materials to high pressure, ranging approximately between 45 and 60 kilobars (4.5 and 6 GPa), but at a comparatively low temperature range between approximately 900 and 1,300 °C (1,650 and 2,370 °F). These conditions are met in two places on Earth; in the lithospheric mantle below relatively stable continental plates, and at the site of a meteorite strike.

Physical Properties of Diamond

Cleavage: {111} Perfect, {111} Perfect, {111} Perfect
Color: Colorless, White, Gray, Black, Blue.
Density: 3.5 – 3.53, Average = 3.51
Diaphaneity: Transparent to Subtransparent to translucent
Fracture: Conchoidal – Fractures developed in brittle materials characterized by smoothly curving surfaces, (e.g. quartz).
Hardness: 10 – Diamond
Luminescence: Fluorescent and phosphorescent blue, Short UV=blue, Long UV=blue.
Luster: Adamantine
Streak: colorless

Photos

A yellow diamond compared to a necklace of almost colorless gems.
Diamond (1.17 carat pale yellow octahedral crystal). Location of mineral deposit: Oranjemund District, southern coastal Namib Desert, Namibia. Overall size of mineral specimen: 6×4.5×4.5 mm. Size of individual crystals: 6 mm. © John Betts – Fine Minerals, New York , NY – All Rights Reserved.
Diamond (0.47 carat fancy-greenish-yellow elongated partial crystal). Location of mineral deposit: Argyle Mine, Kimberley, Western Australia, Australia. Overall size of mineral specimen: 5x3x2.5 mm. Size of individual crystals: 5 mm. © John Betts – Fine Minerals, New York , NY
The diamond immediately right is the Oppenheimer Diamond from Dutoitspan mine, Kimberley, South Africa. It is remarkable not only for its size, 253.7 carats, but also because it has survived uncut. Its double pyramid or octahedral shap is typical of many diamond crystals.