Determining melt productivity of mantle sources from U-238-Th-230 and U-235-Pa-231 disequilibria; an example from Pico Island, Azores
We use coupled 238U-230Th and 235U-231Pa disequilibria measurements from Pico Island, Azores to examine the melting behavior of the underlying mantle. U-series disequilibria in young, mafic lavas are dependent on the melting rate of their source, which in most cases is primarily controlled by its me...
Príomhchruthaitheoirí: | Prytulak, J, Elliott, T |
---|---|
Formáid: | Journal article |
Teanga: | English |
Foilsithe / Cruthaithe: |
2009
|
Míreanna comhchosúla
-
(U-234/U-238) and (Th-230/U-238) disequilibria in fresh and altered Kolbeinsey Ridge basalts
de réir: Elkins, L, et al.
Foilsithe / Cruthaithe: (2009) -
Understanding melt generation beneath the slow-spreading Kolbeinsey Ridge using U-238, Th-230, and Pa-231 excesses
de réir: Elkins, L, et al.
Foilsithe / Cruthaithe: (2011) -
Mantle melting beneath island arcs: U-series constraints from Marianas
de réir: Avanzinelli, R, et al.
Foilsithe / Cruthaithe: (2008) -
U-series disequilibria generated by partial melting of spinel lherzolite
de réir: Landwehr, D, et al.
Foilsithe / Cruthaithe: (2001) -
Determination of 234U/238U, 235U/238U, 236U/238U Isotope Ratios in Uranium Oxide by Sector-Field ICP-MS
de réir: Dmytro V. Kutnii, et al.
Foilsithe / Cruthaithe: (2021-10-01)