In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 20, No. 4 ( 2019-04), p. 1794-1817
Kurzfassung:
Primary magnetic oxides are chrome‐spinel with Fe‐rich exsolution lamellae and magnetite lamellae in pyroxene These carriers are stable at lower crust to uppermost mantle conditions Ultramafic rocks are potential sources of long‐wavelength‐anomalies
Materialart:
Online-Ressource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1029/2018GC008132
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2019
ZDB Id:
2027201-7