Abstract The South Mountain Batholith is a peraluminous granitic complex ranging in
composition from biotite granodiorite to muscovite-topaz 'leucogranite'. Leucogranitic rocks …

ABSTRAC" T The East Kemptville leucogranite, a co. 370 Ma topazmuscovite leucogranite
occurring at the southwest termi nation of the Late Devonian South Mountain Batholith of …

Garnet occurs as a characteristic mineral in granodiorite, monzogranite and leucocratic
monzogranite host rocks near the contact of the South Mountain batholith in Nova Scotia …

Abstract The South Mountain batholith of southwestern Nova Scotia is a large,
peraluminous, granodiorite-granite complex which intrudes mainly greenschist facies …

An occurrence of spessartine-rich (15-25 mole Vo) almandine garnet within a late-stage,
polyphase granitic intrusion (18-20 km2) of the 37GMa-old South Mountain batholith, Nova …

The major-and trace-element chemistry of the mineral constituents of the East Kemptville
leucoglanite reflects chemical equilibration at both the magmatic (muscovite, bulk alkali …

Vertical, W-and NW-trending, post-tectonic, Proterozoic dykes at Napoleon Bay,
southeastern Baffin Island, Northwest Territories, contain mineral assemblages typical of …

ABSTRACT The South Mountain batholith (SMB). of Late Devonian-Earlv Carboniferous ase
(37?-361 Ma\, is an intrusive complex. of peraluminous grano'diorites. monzogranites …

Evaluating the origin of garnet, cordierite, and biotite in granites provides important insight
into closed-and open-system magma evolution. We present field, textural, major-and trace …

Abstract The South Mountain Batholith (SMB) is a peraluminous granitic complex containing
characteristic minerals such as biotite, muscovite, garnet, cordierite, andalusite, ilmenite …