Skip to main content
. Author manuscript; available in PMC: 2020 Dec 2.
Published in final edited form as: Geochim Cosmochim Acta. 2019 Feb 27;251:217–228. doi: 10.1016/j.gca.2019.02.035

Table 1.

Molybdenum and Ru isotopic compositions of Milton, the SBT, and the average value of the SBT parent body.

Sample na μ94Mo ± μ95Mo ± μ97Mo ± na μ100Ru ±
Milton 2 +130 26 +104 9 +54 5 3 −114 15
Babb’s Mill 5 +132 9 +104 5 +46 3 2 −104 9
South Byron 4 +127 12 +104 6 +50 3 3 −111 9
ILD 83500 4 +121 13 +99 9 +50 2 3 −104 10
SBT average 13 +127 7 +103 4 +49 2 8 −107 5
a

n is the number of analyses for Mo and Ru isotopic composition. The reported isotopic values reflect the average values obtained for each meteorite piece. Uncertainties reflect the largest (of n analyses) 2SD of the standards run during an analytical campaign (n ≤ 3) or 2SE (n > 3) of the sample values.