Not exact matches
The amount of nickel - 60 found in
meteorite samples — particularly in comparison to the amount of stable, «ordinary»
iron - 56 — can indicate how much
iron - 60 was present when the larger parent body from
which the
meteorite broke off was formed.
An
iron and silicate
meteorite is thought to resemble the raw material from
which the core formed.
This finding was expected because
meteorites from Vesta have less
iron than the solar nebula from
which planetary building blocks formed.
Besides
iron meteorites,
which were once 1,300 °F, chondrules were once about 3,000 °F.
Figure 3 - An
Iron meteorite, a large sample of
which can be used to reconstruct the past cosmic ray flux variations.