Evidence for southward subduction of the Mongol-Okhotsk oceanic plate: Implications from Mesozoic adakitic lavas from Mongolia (2020)
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.gr.2019.09.007
Publication URI: http://dx.doi.org/10.1016/j.gr.2019.09.007
Type: Journal Article/Review
Parent Publication: Gondwana Research