The contribution of hydrothermally altered ocean crust to the mantle halogen and noble gas cycles
Recent studies suggest that seawater-derived noble gases and halogens are recycled into the deep mantle by the subduction of oceanic crust. To understand the processes controlling the availability of halogens and noble gases for subduction, we determined the noble gas elemental and isotopic ratios a...
Main Authors: | Chavrit, D, Burgess, R, Sumino, H, Teagle, D, Droop, G, Shimizu, A, Ballentine, C |
---|---|
Format: | Journal article |
Published: |
Elsevier
2016
|
Similar Items
-
Seawater-derived noble gases and halogens preserved in exhumed mantle wedge peridotite
by: Sumino, H, et al.
Published: (2010) -
Sedimentary halogens and noble gases within Western Antarctic xenoliths: Implications of extensive volatile recycling to the sub continental lithospheric mantle
by: Broadley, M, et al.
Published: (2015) -
Slab-derived halogens and noble gases illuminate closed system processes controlling volatile element transport into the mantle wedge
by: Kobayashi, M, et al.
Published: (2016) -
Halogen Heterogeneity in the Lithosphere and Evolution of Mantle Halogen Abundances Inferred From Intraplate Mantle Xenoliths
by: Kobayashi, M, et al.
Published: (2019) -
Noble gases in mantle plumes.
by: Ballentine, C, et al.
Published: (2001)