Details
This partial slice of a meteorite features a mosaic of sparkling olivine and peridot in a gleaming iron-nickel matrix, etched to reveal the crystalline structure. On custom stand.
234 x 2in. (6.9 x 5.3 x 0.2cm.)
314in. (8cm.) high on stand.
40g.
Special notice
Specified lots are being stored at Crozier Park Royal (details below) or will be removed from Christie’s, 8 King Street, London, SW1Y 6QT by 5.00pm on the day of the sale. Christie’s will inform you if the lot has been sent offsite. If the lot has been transferred to Crozier Park Royal, it will be available for collection from 12.00pm on the second business day following the sale. Please call Christie’s Client Service 24 hours in advance to book a collection time at Crozier Park Royal. All collections from Crozier Park Royal will be by pre-booked appointment only. Tel: +44 (0)20 7839 9060 Email: cscollectionsuk@christies.com. If the lot remains at Christie’s, 8 King Street, it will be available for collection on any working day (not weekends) from 9.00am to 5.00pm
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Lot Essay

Pallasites are not only rare, representing less than 0.2% of all known meteorites, they are also widely considered the most beautiful extraterrestrial substance known—and samples of Fukang are among the most coveted. This slice is one of the largest cut from the Fukang main mass. Recovered in China’s Gobi Desert, this extraordinary meteorite contains some of the largest and most translucent crystals of any pallasite. Comprised of approximately 50% olivine and peridot (gem-quality olivine) crystals suspended in a nickel-iron matrix. Main-group pallasites originated from the mantle-core boundary of an asteroid formed 4.5 billion years ago in the early Solar System. During the early chaos of planetary collisions, that asteroid broke apart after an enormously energetic impact with another asteroid, before later falling to Earth in a fiery descent.

The pallasite appellation for this meteorite class is in honor of the German scientist, Peter Simon Pallas (1741-1811), who while traveling through Siberia, examined the first pallasitic mass in the early 1770s. This is an honour Pallas is fortunate to have received, for he believed the unusual specimen he examined could not possibly have come from outer space.

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