Results 171 to 180 of about 40,246 (197)
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D-depleted organic matter and graphite in the Abee enstatite chondrite

, 2012
L. Remusat   +5 more
semanticscholar   +1 more source

Evolution of the Parent Body of Enstatite (EL) Chondrites

Icarus, 2022
Hans-Peter Gail   +2 more
exaly  

Olivine in EH Chondrites as an indicator of metamorphism in the enstatite chondrite parent body

2013
High-Fe enstatite chondrites (EH chondrites) are samples of planetesimals accreted in a region of the solar nebula with very low oxygen fugacity [1]. A consequence of this reduction is that Fe exists as metal rather than as FeO in silicates, with pyroxene rather than olivine being the most common mineral (stabilized by low (FeO+MgO)/SiO2) [1, 2].
McKibbin, Seann   +3 more
openaire   +1 more source

Oxygen Isotopes in Calcium–Aluminum-Rich Inclusions From Enstatite Chondrites: New Evidence for a Single CAI Source in the Solar Nebula

Earth and Planetary Science Letters, 2000
Kevin D. McKeegan   +2 more
exaly  

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