Assessment of magmatic vs. metasomatic processes in rare-metal granites: A case study of the Cínovec/Zinnwald Sn – W – Li deposit, Central Europe
| Authors | |
|---|---|
| Year of publication | 2017 |
| Type | Article in Periodical |
| Magazine / Source | Lithos |
| MU Faculty or unit | |
| Citation | |
| Doi | https://doi.org/10.1016/j.lithos.2017.08.015 |
| Field | Analytic chemistry |
| Keywords | Rare-metal granite; Cínovec/Zinnwald deposit; Rock textures; Metasomatic processes; Magmatic processes |
| Description | The Cínovec rare-metal granite in the eastern segment of the Krušné Hory/Erzgebirge (Czech Republic/Germany)formed in the final stage of the magmatic evolution of the late Variscan volcano-plutonic system known as the Teplice caldera. The granite is slightly peraluminous; enriched in F, Li, Rb, Cs, Nb, Ta, Sn, W, Sc and U; and poor in P, Mg, Ti, Sr and B. |
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