An Amoeboid Olivine Aggregate Surrounded by an Igneous Ferroan Olivine-Rich Rim from CO3.0 Chondrite DOM 08006

· by · in , ,

K. Nagashima, A. N. Krot, C. Park

46th Lunar and Planetary Science Conference (2015), Abstract #2477

PDF LINK

Related posts (automatically generated):

  1. Microstructural constraints on complex thermal histories of refractory CAI-like objects in an amoeboid olivine aggregate from the ALHA77307 CO3.0 chondrite
  2. LIME silicates in amoeboid olivine aggregates in carbonaceous chondrites: Indicator of nebular and asteroidal processes
  3. A record of low-temperature asteroidal processes of amoeboid olivine aggregates from Kainsaz CO3.2 chondrite
  4. Microstructural evidence for complex formation histories of amoeboid olivine aggregates from the ALHA77307 CO3.0 chondrite
  5. Formation of CV chondrules by recycling of amoeboid olivine aggregate-like precursors
  6. Genetic relationship between Na-rich chondrules and Ca,Al-rich inclusions? – Formation of Na-rich chondrules by melting of refractory and volatile precursors in the Solar Nebula
  7. Condensate refractory inclusions from the CO3.00 chondrite Dominion Range 08006: Petrography, mineral chemistry, and isotopic compositions
  8. Amoeboid olivine aggregates from CH carbonaceous chondrites
  9. Correlated isotopic and chemical evidence for condensation origins of olivine in comet 81P/Wild 2 and in AOAs from CV and CO chondrites
  10. Chondrule heritage and thermal histories from trace element and oxygen isotope analyses of chondrules and amoeboid olivine aggregatesOPEN ACCESS 
Tags: , ,