Iron and zinc stable isotope evidence for open-system high-pressure dehydration of antigorite serpentinite in subduction zones (2021)
Attributed to:
Mantle volatiles: processes, reservoirs and fluxes
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.17863/cam.62014
Publication URI: https://www.repository.cam.ac.uk/handle/1810/314908
Type: Journal Article/Review