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Late-Variscan metaluminous/weakly peraluminous (quartz-diorites and tonalites) and strongly peraluminous (two mica porphyritic granodiorites and granites) granitoids represent two magmatic associations making up the Capo Vaticano Promontory (central Calabria, Italy). They characterize a portion of a complete continental crustal section exposed in c...
The granitoids of the Serre Batholith make up the middle portion of an entire section of late Variscan continental crust exposed in the central Calabria. The most felsic rock types consist of two-mica K-feldspar megacrystic granodiorites and granites (BMPG), passing southward to two-mica granodiorites and granites (BMG), that grade further south to...
Weakly to strongly peraluminous granodiorites and granites represent the most felsic rocks of the Serre Batholith, which makes up the intermediate portion (c. 13 km thick) of a nearly complete cross section of continental crust exposed in central Calabria. These rocks are Bt±Am granodiorites (BAG), two-mica granodiorites and granites (BMG) and two-...
The late Variscan granitoids of the Serre Batholith form the middle portion of an entire crustal section exposed in central Calabria. The most felsic rock types consist of two-mica K-feldspar megacrystic granodiorites and granites (BMPG), passing southward to slightly inequigranular two-mica granodiorites and granites (BMG), that grade further sout...
