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  Distribution of 26Al in the solar system (Makide+, 2011)
Post annotation
1.J/ApJ/733/L31/table1Oxygen-isotope compositions and the inferred (26Al/27Al)0 ratios from individual micron-sized corundum grain in unequilibrated ordinary chondrites (UOCs) and unmetamorphosed CM carbonaceous chondrites (CCs) (116 rows)

Query by Constraints constraints help applied on Columns (Output Order: + - )
ShowSortColumn  Constraint Explain   (UCD)
  recno  Record number assigned by the VizieR team. Should Not be used for identification. (meta.record)
  Type (char) chondrite type (Carbonaceus or Ordinary) (src.class)
  Grain (char) Grain (Note 1)   (;meta.main)
  d18O 10-3 Excess δ18O of 18O isotope (phys.abund)
  e_d18O 10-3 The 2σ error in d180 (stat.error)
  d17O 10-3 Excess δ18O of 17O isotope (phys.abund)
  e_d17O 10-3 The 2σ error in d170 (stat.error)
  D17O 10-3 Δ17O composition (D17O=d17O-0.52*d18O) (phys.abund)
  e_D17O 10-3 The 2σ error in D17O (stat.error)
  Al.r 10-5 (n) Inferred (26Al/27Al)0 ratio (Note 2)   (phys.abund)
  e_Al.r 10-5 (n) The 2σ error in Al.r (stat.error)

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