Table 1 Statistical information on the fitting of the PDF peaks as a function of pressure.
From: Tetracarbonates in silicate melts may be at the origin of a deep carbon reservoir in the deep Earth
P (GPa) | C-O (Å) | Mg-O (Å) | K-O (Å) | C-O (FWHM) |
|---|---|---|---|---|
0 | 1.243 (2) | 2.097 (2) | 2.848 (6) | 0.2915 |
33 (2) | 1.185 (2) | 1.939 (7) | 2.621 (1) | 0.3372 |
46 (3) | 1.236 (1) | 1.937 (3) | 2.471 (2) | 0.3144 |
85 (4) | 1.323 (1) | 1.979 (45) | 2.406 (23) | 0.3709 |
104 (4) | 1.191 (3) | 1.982 (8) | 2.381 (3) | 0.4381 |
