Skip to main content
Fig. 17 | Swiss Journal of Geosciences

Fig. 17

From: The Val Biandino Intrusive Suite (central Southern Alps, N Italy): new geochronological and geochemical data on the Early Permian magmatic activity in the Southalpine Domain

Fig. 17

Composition of the cordierite granites of the VBQD and of granites of the VSBG compared with the compositions of possible rock sources. Most of the rock samples display LILE abundance and ratios (Rb/Ba, Rb/Sr, Ba). Also in terms of major elements (K, and and Ca, d), the VBQD and VSBG granites suggest the contribution of partial melting of metapelites and metapsammites during their genesis. Data of the Variscan S-type granites are from Finger & Schiller (2012)

Back to article page