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An iron peak element is an element with an atomic number in the vicinity of iron's (26), i.e., the vicinity of the iron peak:
symbol | element | atomic number |
titanium | Ti | 22 |
vanadium | V | 23 |
chromium | Cr | 24 |
manganese | Mn | 25 |
iron | Fe | 26 |
cobalt | Co | 27 |
nickel | Ni | 28 |
Scandium, Sc, 21 is also sometimes treated as one. A common astrophysics classification of (somewhat heavy) elements is as either an iron peak element or an alpha element, even though the even-numbered iron peak elements can be produced by the alpha process. The distinction is made because some types of supernova tend to produce a lot more iron peak elements relative to alpha elements, i.e., the relative abundances of the two groups reveal information of past supernovae and star formation history.