# Fukang meteorite - Page: https://taslar.bumba.tr/en/stones/fukang-meteorite/ - Turkish: Fukang meteoriti - Also known as: Fukang pallasite - Kind: Meteorite - Classification: Meteorites and impact stones › Stony-iron meteorites - Hardness (Mohs): 4–7 - Specific gravity: 4.66–4.86 g/cm³ - Lustre: Metallic, Vitreous (glassy) - Transparency: Opaque, Translucent - Colours: golden yellow to olive green (olivine crystals), silvery grey (metal) - Composition: Main-group pallasite: large olivine (peridot) crystals in nickel–iron metal. The metal is 89.9% iron, 9.0% nickel, 0.62% phosphorus and 0.51% cobalt; the olivine is magnesium-rich (Fo 86.4). The metal is mostly kamacite (6.98% nickel on average), and some olivine holds vermicular troilite. - Texture: The olivine crystals range from rounded to angular and from under 5 millimetres to several centimetres; many are fractured. The main mass has clusters of massive olivine up to 11 cm across, cut by thin metal veins. - Value ladder: 7/9 step, Precious stone A stained-glass window from space: a one-tonne pallasite from China with gem-quality peridot crystals set in silvery metal. The Fukang meteorite is a 1,003-kilogram pallasite found in 2000 in the mountains near Fukang, in China's Xinjiang region. Pallasites are stony-iron meteorites made of olivine crystals set in nickel–iron metal. Fukang's olivines are large and gem quality (peridot); when thin slices are lit from behind, the crystals glow golden and green. It is estimated to be about 4.5 billion years old. ## How does it form? Pallasites are thought to form at the boundary where an asteroid's molten metal core meets its olivine-rich rocky mantle. There olivine crystals became embedded in molten nickel–iron, and when the metal cooled and solidified the crystals were trapped inside. Fukang is a "main-group" pallasite. Fukang's metal is mostly kamacite. It is estimated to be about 4.5 billion years old, close to the age of the Solar System. After the parent body was broken up by collisions, a piece reached Earth; its fall was not seen. ## What is it used for? Fukang was studied at the University of Arizona's Southwest Meteorite Center by Dante Lauretta and his team, joined by Ian Franchi of the Open University. Pallasites are studied to understand the inner structure of asteroids, the boundary between metal core and mantle, and how these bodies cooled. The oxygen isotope ratios of the olivine help show which group of pallasites a meteorite belongs to. Thin slices cut from Fukang are among the most admired meteorite specimens in museums and collections. ## Specimens A 31-kilogram section is kept at the University of Arizona as the type specimen. The main mass has been displayed in the University of Arizona's Michael J. Drake building. ## How to recognise it - Translucent crystals ranging from golden yellow to olive green, set in silvery grey metal. - The crystals range from rounded to angular and from under 5 millimetres to several centimetres, and many are fractured. - The metal makes it heavy; only documentation and laboratory analysis can show that a slice really comes from Fukang. ## What determines its value? Pallasites are a very small share of meteorites, and the coloured olivine crystals revealed when they are cut make them among the most sought-after meteorites for collectors. A slice's value depends on the clarity, colour and soundness of its olivines, how thin and large the slice is, how well the metal resists rust, and its documented origin. This information is educational, not buying, selling or investment advice. Value varies enormously with quality and treatment. ## Myths and misconceptions - Myth: Peridot is a gemstone that forms only on Earth. Fact: Peridot is gem-quality olivine, and it also occurs in pallasites such as Fukang. Fukang's large olivine crystals come from a piece of a 4.5-billion-year-old asteroid. - Myth: The main mass of Fukang was sold at auction. Fact: The main mass was offered at a Bonhams auction in New York in April 2008, but it did not sell. Part of the mass and a research specimen are at the University of Arizona. ## Curious questions **What are the green crystals in the Fukang meteorite?** They are olivine crystals; gem-quality olivine is called peridot. Fukang's olivine is rich in magnesium. The crystals formed where an asteroid's metal core met its rocky mantle, becoming embedded in molten metal. ## Did you know? - The Chinese dealer who obtained the mass removed about 20 kg from it; in 2005 it was brought to the Tucson Gem and Mineral Show, where the planetary scientist Dante Lauretta spotted it. - The main mass contains clusters of massive olivine up to 11 centimetres across, cut by thin metal veins. - A 48 × 91 centimetre “window” was cut and polished into the main mass to give a view into its gem-quality areas. ## Where is it found? - Mountains near Fukang, Xinjiang, China (Type locality): The area where the 1,003-kilogram mass was found in 2000; its fall was not observed. ## Sources - [Fukang meteorite](https://en.wikipedia.org/wiki/Fukang_meteorite), Wikipedia - [Fukang meteoriti](https://tr.wikipedia.org/wiki/Fukang_meteoriti), Vikipedi - [Pallasite](https://en.wikipedia.org/wiki/Pallasite), Wikipedia - [Meteorite porosities and densities: a review of trends in the data (D. T. Britt & G. J. Consolmagno), Lunar and Planetary Science XXXV, abstract 2108](https://www.lpi.usra.edu/meetings/lpsc2004/pdf/2108.pdf), Lunar and Planetary Institute, 2004 - [Kamacite Mineral Data](http://webmineral.com/data/Kamacite.shtml), Webmineral.com - [Handbook of Mineralogy: Forsterite](https://www.handbookofmineralogy.org/pdfs/forsterite.pdf), Mineralogical Society of America Source: https://taslar.bumba.tr/en/stones/fukang-meteorite/ · Licence: CC BY-SA 4.0