Oxygen Isotope Ratios of Magnetite in CI-Like Clasts from a Polymict Ureilite

· by · in

Kita N. T. * Defouilloy C. Goodrich C. A. Zolensky M. E.

80th Annual Meeting of the Meteoritical Society 2017 [#6153]

abstract (PDF)

“Magnetites in CI-like dark clasts in polymict ureilite show significant depletion in 16O with Δ17O=+5‰. They are either xenolitic materials to UPB that are not known as meteorites, or represent hydrated precursors of ureilites.”

Related posts (automatically generated):

  1. Melt Formation and Evolution on the Ureilite Parent Body, as Shown by Feldspathic Clasts in Polymict Ureilites
  2. Mineralogy and oxygen isotope systematics of magnetite grains and a magnetite‐dolomite assemblage in hydrated fine‐grained Antarctic micrometeorites
  3. 40Ar/39Ar ages of L4, H5, EL6, and feldspathic ureilitic clasts from the Almahata Sitta polymict ureilite (asteroid 2008 TC3)OPEN ACCESS 
  4. O-Isotope Composition of CI- and CM-Like Clasts in Ureilites, HEDs, and CR Chondrites
  5. Almahata Sitta is No More Exotic Than any Other Polymict Ureilite
  6. Mineralogy, petrology, and oxygen‐isotope compositions of magnetite ± fayalite assemblages in CO3, CV3, and LL3 chondrites
  7. Enstatite meteorite clasts in Almahata Sitta and other polymict ureilites: Implications for the formation of asteroid 2008 TC3 and the history of enstatite meteorite parent asteroids
  8. O-Isotope Signatures of Olivine and Pyroxene Grains in C1 and CM-Like Clasts
  9. Mineralogy of volatile‐rich clasts in brecciated meteorites
  10. Petrology and oxygen isotopic compositions of clasts in HED polymict breccia NWA 5232.
Tags: , , , ,