Cited by 58Astro and Planetary ScienceHigh-pressure geophysics and materialsDiamond and Carbon-based Materials Research

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Impact shock origin of diamonds in ureilite meteorites

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Abstract

Significance: The origin of diamonds in ureilites is still a debated issue among the scientific community, with significant implications for the sizes of early Solar System bodies. We investigated three diamond-bearing ureilites by a multimethodological approach using scanning electron microscopy, micro X-ray diffraction, transmission electron microscopy, and micro-Raman spectroscopy, with the aim of determining the origin of the diamonds. Our results show that formation of both microdiamonds and nanodiamonds in ureilites can be explained by impact shock events on a small planetesimal and does not require long growth times at high static pressures within a Mercury- or Mars-sized body.

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Crossref · 10.1073/pnas.1919067117

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References 77 · Cited by 58

Research works printed but not linked: 2

  1. C. A. Goodrich, Invited review. Ureilites: A critical review. Meteorit. Planet. Sci. 352, 327–352 (1992).
  2. T. D. Varfolomeeva “Synthesis and investigation of polycrystalline diamond ” PhD thesis Institute for High Pressure Physics USSR Academy of Sciences (1971) p. 154.

Metadata

Authors
Nestola, F., Goodrich, C. A., Morana, M., Barbaro, A., Jakubek, R. S., Christ, O., Brenker, F. E., Domeneghetti, M. C., Dalconi, M. C., Alvaro, M., Fioretti, A. M., Litasov, K. D., Fries, M. D., Leoni, M., Casati, N. P. M., Jenniskens, P., & Shaddad, M. H.
Affiliations
  • Goethe University Frankfurt (DE)
  • Universities Space Research Association (US)
  • University of Pavia (IT)
  • National Aeronautics and Space Administration (US)
  • University of Padua (IT)
  • Institute of Geosciences and Earth Resources (IT)
  • Institute for High Pressure Physics (RU)
  • University of Trento (IT)
  • Paul Scherrer Institute (CH)
  • Search for Extraterrestrial Intelligence (US)
  • University of Khartoum (SD)
Corresponding author
  • Nestola, Fabrizio
  • Goodrich, Cyrena A.
Venue
Proceedings of the National Academy of Sciences
Published
2020-09-28
Volume
117
Issue
41
Pages
25310-25318
ISSN
  • 0027-8424 (ISSN-L)
  • 1091-6490
OpenAlex
W3089646553
Cited by
58
References
77
Citations by year
2026: 8 · 2025: 12 · 2024: 10 · 2023: 8 · 2022: 11 · 2021: 8 · 2020: 1
FWCI
3.12
Type
journal article
Language
en
Open access
Locations
  • Proceedings of the National Academy of Sciences (publishedVersion, cc-by-nc-nd)
  • PubMed Central (publishedVersion, cc-by-nc-nd)
  • PubMed (publishedVersion)
  • DORA PSI (Paul Scherrer Institute) (submittedVersion, cc-by-nc-nd)
  • Padua Research Archive (University of Padova) (submittedVersion, cc-by-nc-nd)
  • Florence Research (University of Florence) (submittedVersion, other-oa)
  • Institutional Research Information System (Università degli Studi di Trento) (submittedVersion)
  • USRA Houston Repository (Lunar and Planetary Institute) (submittedVersion, cc-by-nc-nd)
Funders
  • NASA (NASA grants 80NSSC17K0165, NNX17AH09GS03, and 80NSSC19K0507)
  • Ministero dell'Istruzione, dell'Università e della Ricerca (R164WEJAHH)
  • PNRA (PNRA 2016, PNRA18 00247-A)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Astro and Planetary Science
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
  • Physical Sciences › Materials Science › Materials Chemistry › Diamond and Carbon-based Materials Research
Keywords
diamond formation, ureilite meteorites, shock metamorphism, nanodiamonds, graphite-to-diamond transformation, Almahata Sitta, single-crystal diamond, pseudomorphism, Mars, mercury

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