Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6440744 | Lithos | 2015 | 8 Pages |
Abstract
The figure represents the pressure of entrapment of garnet by the diamond (i.e. the pressure of formation of the pair) as a function of the pyrope content for a pyrope-almandine inclusion in diamond. The black squares correspond to the data calculated with our new thermo-elastic parameters along thr pyrope-almandine join. Bulk moduli above 170Â GPa for pyrope would confirm that our value lower than 165Â GPa is more realistic than the previous one.54
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
S. Milani, F. Nestola, M. Alvaro, D. Pasqual, M.L. Mazzucchelli, M.C. Domeneghetti, C.A. Geiger,