Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6443013 | Earth-Science Reviews | 2014 | 15 Pages |
Abstract
On the basis of thermodynamic equilibrium data for C-H-O fluids in the mantle we argue that submicron inclusions in diamonds are products of local remobilization connected to fluid-fluxed partial melting and redox freezing. Thus, evidence from these inclusions complements information from classical work on larger inclusions and allows a unique direct insight into the medium in which diamond formed.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Dorrit E. Jacob, Larissa Dobrzhinetskaya, Richard Wirth,