Details
| Original language | English |
|---|---|
| Pages (from-to) | 1600-1601 |
| Number of pages | 2 |
| Journal | SCIENCE |
| Volume | 320 |
| Issue number | 5883 |
| Publication status | Published - 20 Jun 2008 |
| Externally published | Yes |
Abstract
Unlike other metals, magmatic melting and recrystallization fractionate iron isotopes, possibly because of the different oxidation states of iron.
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In: SCIENCE, Vol. 320, No. 5883, 20.06.2008, p. 1600-1601.
Research output: Contribution to journal › Survey paper › Research › peer review
}
TY - JOUR
T1 - What drives iron isotope fractionation in magma?
AU - Weyer, Stefan
PY - 2008/6/20
Y1 - 2008/6/20
N2 - Unlike other metals, magmatic melting and recrystallization fractionate iron isotopes, possibly because of the different oxidation states of iron.
AB - Unlike other metals, magmatic melting and recrystallization fractionate iron isotopes, possibly because of the different oxidation states of iron.
UR - http://www.scopus.com/inward/record.url?scp=46449134781&partnerID=8YFLogxK
U2 - 10.1126/science.1160204
DO - 10.1126/science.1160204
M3 - Survey paper
AN - SCOPUS:46449134781
VL - 320
SP - 1600
EP - 1601
JO - SCIENCE
JF - SCIENCE
SN - 0036-8075
IS - 5883
ER -