O and H isotopic evidence for a mantle source of water in appinite magma: An example from the late Neoproterozoic Greendale Complex, Nova Scotia (2021)
Attributed to:
National Environmental Isotope Facility (NEIF)
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1016/j.lithos.2021.105997
Publication URI: http://dx.doi.org/10.1016/j.lithos.2021.105997
Type: Journal Article/Review
Parent Publication: Lithos