Abstract
Predazzo Magmatic Complex represents the main intrusive boby o the magmatic activity which affected the South Alpine domain during the Triassic age (238-232 My).
Field observations and petrological data allow to distinguish four main intrusive sequences characterised by a clear subduction-related signature: a shoshontic SiO2-saturated series (M1); a shoshtonic SiO2-oversaturated series (M2); a K-alkine SiO2-undersaturated series (M3) and a Grantic Unit (G).
Field observations and petrological data allow to distinguish four main intrusive sequences characterised by a clear subduction-related signature: a shoshontic SiO2-saturated series (M1); a shoshtonic SiO2-oversaturated series (M2); a K-alkine SiO2-undersaturated series (M3) and a Grantic Unit (G).
| Original language | English |
|---|---|
| Pages (from-to) | 486-486 |
| Number of pages | 1 |
| Journal | Geochimica et Cosmochimica Acta |
| Volume | 66 |
| Issue number | 15, Supplement |
| DOIs | |
| Publication status | Published - Aug 2002 |
| Externally published | Yes |
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