Research output: Contribution to journal › Article › peer-review
Vlodavetsite is a product of fumarole activity associated with the Great Tolbachik fissure eruption in Kamchatka in 1974 and 1976. This is always accompanied by fine-particle pyroclastic material. By using a RGNS X-ray goniometer and an automatic Syntex-P21 diffractometer, it is shown that vlodavetsite single crystals belong to the tetragonal system, the point group 4/m and the diffraction group I-/-(law of hkl maxima, h + k + 1 = 2n).
| Original language | English |
|---|---|
| Pages (from-to) | 173-176 |
| Number of pages | 4 |
| Journal | Transactions (Doklady) of the Russian Academy of Sciences. Earth science sections. |
| Volume | 345 |
| Issue number | 8 |
| State | Published - 1 Aug 1996 |
ID: 53955808