Table 1 Activation energy Ea for single-crystal amphiboles, covering a broad range of Fe/(Fe + Mg) ratios, as reported in the literature.
Method | Sample identification | Fe/(Fe + Mg) | Ea (eV) | References |
---|---|---|---|---|
Impedance spectroscopy | arfvedsonite | ~ 1 | 0.4 (σ||) | Schmidbauer et al.24 |
edenitic-hornblende | 0.75 | 0.58 (σ||) | Schmidbauer et al.25 | |
edenite | 0.36 | 0.70–0.80 | Hu et al.22 | |
kaersutite | 0.25 | 0.61 (σ||) | Schmidbauer et al.25 | |
Mg-hornblende | 0.22 | 0.73–1.06 (σ||) | Schmidbauer et al.25 | |
tremolite | 0.01 | 3.79 | Shen et al.31 | |
dc electrical resistance | riebeckite (crocidolite) | ~ 1* | 0.69 (σ||) | Littler and Williams43 |
riebeckite | ~ 1* | 0.9 (σ||) | Parkhomenko45 | |
riebeckite | 0.95 | 0.77 (σ||) | Della Ventura et al.26 | |
riebeckite | 0.95 | 0.53 (σ||) (300–720 K) | This work | |
not given | 0.19 | 0.54(σ||) and 0.57(σ⊥) | Tolland27 |