Origin of micrometer-sized impact diamonds in ureilites by catalytic growth involving Fe-Ni-silicide: The example of Kenna meteorite

Author:

Barbaro AnnaORCID,Domeneghetti Maria Chiara,Litasov Konstantin D.,Ferrière LudovicORCID,Pittarello Lidia,Christ OliverORCID,Lorenzon Sofia,Alvaro Matteo,Nestola Fabrizio

Funder

MIUR

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference66 articles.

1. The constitution of the ternary system Fe–Ni–Si;Ackerbauer;Intermetallics,2009

2. Graphite based geothermometry on Almahata Sitta ureilites meteorites;Barbaro;Minerals,2020

3. Characterization of carbon phases in Yamato 74123 ureilite to constrain the meteorite shock history;Barbaro;Am. Mineral.,2021

4. The Kenna ureilite: an ultramafic rock with evidence for igneous, metamorphic, and shock origin;Berkley;Geochim. Cosmochim. Acta,1976

5. The magnetic effects of brecciation and shock in meteorites: II. The ureilites and evidence for strong nebular magnetic fields;Brecher;Moon Planets,1979

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