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20 April 2024
 
  » pubmed » pmid17170295

 Article overview


Mineralogy and petrology of comet 81P/Wild 2 nucleus samples
Michael E Zolensky ; Thomas J Zega ; Hajime Yano ; Sue Wirick ; Andrew J Westphal ; Mike K Weisberg ; Iris Weber ; Jack L Warren ; Michael A Velbel ; Akira Tsuchiyama ; Peter Tsou ; Alice Toppani ; Naotaka Tomioka ; Kazushige Tomeoka ; Nick Teslich ; Mitra Taheri ; Jean Susini ; Rhonda Stroud ; Thomas Stephan ; Frank J Stadermann ; Christopher J Snead ; Steven B Simon ; Alexandre Simionovici ; Thomas H See ; François Robert ; Frans J M Rietmeijer ; William Rao ; Murielle C Perronnet ; Dimitri A Papanastassiou ; Kyoko Okudaira ; Kazumasa Ohsumi ; Ichiro Ohnishi ; Keiko Nakamura-Messenger ; Tomoki Nakamura ; Smail Mostefaoui ; Takashi Mikouchi ; Anders Meibom ; Graciela Matrajt ; Matthew A Marcus ; Hugues Leroux ; Laurence Lemelle ; Loan Le ; Antonio Lanzirotti ; Falko Langenhorst ; Alexander N Krot ; Lindsay P Keller ; Anton T Kearsley ; David Joswiak ; Damien Jacob ; Hope Ishii ; Ralph Harvey ; Kenji Hagiya ; Lawrence Grossman ; Jeffrey N Grossman ; Giles A Graham ; Matthieu Gounelle ; Philippe Gillet ; Matthew J Genge ; George Flynn ; Tristan Ferroir ; Stewart Fallon ; Sirine Fakra ; Denton S Ebel ; Zu Rong Dai ; Patrick Cordier ; Benton Clark ; Miaofang Chi ; Anna L Butterworth ; Donald E Brownlee ; John C Bridges ; Sean Brennan ; Adrian Brearley ; John P Bradley ; Pierre Bleuet ; Phil A Bl ; Ron Bastien ;
Date 15 Dec 2006
Journal Science, 314 (5806), 1735-9
AbstractThe bulk of the comet 81P/Wild 2 (hereafter Wild 2) samples returned to Earth by the Stardust spacecraft appear to be weakly constructed mixtures of nanometer-scale grains, with occasional much larger (over 1 micrometer) ferromagnesian silicates, Fe-Ni sulfides, Fe-Ni metal, and accessory phases. The very wide range of olivine and low-Ca pyroxene compositions in comet Wild 2 requires a wide range of formation conditions, probably reflecting very different formation locations in the protoplanetary disk. The restricted compositional ranges of Fe-Ni sulfides, the wide range for silicates, and the absence of hydrous phases indicate that comet Wild 2 experienced little or no aqueous alteration. Less abundant Wild 2 materials include a refractory particle, whose presence appears to require radial transport in the early protoplanetary disk.
Source PubMed, pmid17170295 doi: 10.1126/science.1135842
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