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 |
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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 |