Timescales of crystal mush mobilization in the Bárðarbunga-Veiðivötn volcanic system based on olivine diffusion chronometry (2021)
Attributed to:
How did primordial and recycled geochemical signatures come to coexist in the Earth's deep mantle?
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.2138/am-2021-7670
Publication URI: http://dx.doi.org/10.2138/am-2021-7670
Type: Journal Article/Review
Parent Publication: American Mineralogist
Issue: 7