Hostname: page-component-848d4c4894-pjpqr Total loading time: 0 Render date: 2024-06-16T10:52:04.177Z Has data issue: false hasContentIssue false
  • English
  • Français

Record of Alteration by Heavy Ices in a Cometary Clast in a Primitive Meteorite

Published online by Cambridge University Press:  30 July 2021

Katherine Burgess ,
Rhonda Stroud ,
Larry Nittler  and
Josep Trigo-Rodriguez
Katherine Burgess
Affiliation:
U.S. Naval Research Laboratory, District of Columbia, United States
Rhonda Stroud
Affiliation:
U.S. Naval Research Laboratory, United States
Larry Nittler
Affiliation:
Carnegie Institution of Washington, United States
Josep Trigo-Rodriguez
Affiliation:
Meteorites, Minor Bodies and Planetary Sciences Group, Institute of Space Sciences (CSIC-IEEC), Barcelona, Catalonia, Spain, Catalonia, Spain

Abstract

An abstract is not available for this content so a preview has been provided. As you have access to this content, a full PDF is available via the ‘Save PDF’ action button.
Image of the first page of this content. For PDF version, please use the ‘Save PDF’ preceeding this image.'
Type
Moon Dust, Minerals and Microscopy
Information
Microscopy and Microanalysis , Volume 27 , Supplement S1 , August 2021 , pp. 2268 - 2270
Check for updates
Copyright
Copyright © The Author(s), 2021. Published by Cambridge University Press on behalf of the Microscopy Society of America

References

Nittler, L. R. et al. A cometary building block in a primitive asteroidal meteorite. Nat. Astron. 3, 659-666, doi:10.1038/s41550-019-0737-8 (2019).CrossRefGoogle Scholar
Sakamoto, N. et al. Remnants of the early Solar System water enriched in heavy oxygen isotopes. Science 317, 231-233, doi:10.1126/science.1142021 (2007).CrossRefGoogle ScholarPubMed
Seto, Y. et al. Mineralogical characterization of a unique material having heavy oxygen isotope anomaly in matrix of the primitive carbonaceous chondrite Acfer 094. Geochim. Cosmochim. Acta 72, 2723-2734, doi:10.1016/j.gca.2008.03.010 (2008).CrossRefGoogle Scholar
Starkey, N. A., Franchi, I. A. & Lee, M. R. Isotopic diversity in interplanetary dust particles and preservation of extreme 16O-depletion. Geochim. Cosmochim. Acta 142, 115-131, doi:10.1016/j.gca.2014.07.011 (2014).CrossRefGoogle Scholar
Yabuta, H. et al. Formation of an ultracarbonaceous Antarctic micrometeorite through minimal aqueous alteration in a small porous icy body. Geochim. Cosmochim. Acta 214, 172-190, doi:10.1016/j.gca.2017.06.047 (2017).CrossRefGoogle Scholar
Trigo-Rodríguez, J. M., Llorca, J. & Fabregat, J. Chemical abundances determined from meteor spectra — II. Evidence for enlarged sodium abundances in meteoroids. Mon Not R Astron Soc 348, 802-810, doi:10.1111/j.1365-2966.2004.07389.x (2004).CrossRefGoogle Scholar
Bradley, J. P. et al. Detection of solar wind-produced water in irradiated rims on silicate minerals. Proc. Nat. Acad. Sci. 111, 1732-1735, doi:10.1073/pnas.1320115111 (2014).CrossRefGoogle ScholarPubMed
Garvie, L. A. J. & Buseck, P. R. Prebiotic carbon in clays from Orgueil and Ivuna (CI), and Tagish Lake (C2 ungrouped) meteorites. Meteor. Planet. Sci. 42, 2111-2117, doi:10.1111/j.1945-5100.2007.tb01011.x (2007).CrossRefGoogle Scholar