Details
| Originalsprache | Englisch |
|---|---|
| Seiten (von - bis) | 1600-1601 |
| Seitenumfang | 2 |
| Fachzeitschrift | SCIENCE |
| Jahrgang | 320 |
| Ausgabenummer | 5883 |
| Publikationsstatus | Veröffentlicht - 20 Juni 2008 |
| Extern publiziert | Ja |
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, Jahrgang 320, Nr. 5883, 20.06.2008, S. 1600-1601.
Publikation: Beitrag in Fachzeitschrift › Survey Paper › Forschung › 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 -