ABSTRACT The Meguma Zone of southern Nova Scotia docked with North America in the
mid-Late Devonian. Associated magmatic activity involved small calc-alkaline lamprophyric …

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

ABSTRACT The Peggys Cove area of southern Nova Scotia contains abundant, flat-lying,
zoned, tourmaline-bearing aplite–pegmatite sheets cutting leucomonzogranite of the …

Granitic plutons in the Meguma Terrane may be broadly divided into two suites:(1) an areally
predominant, cogenetic suite of peraluminous granitoid rocks (tonalite-leucogranite); and (2) …

The reservoir characterization and provenance of the Wolfville Formation were investigated
using petrography, heavy minerals and microprobe analysis of tourmaline and garnet …

Successive and superimposed periods of late-to post-magmatic metasomatism have
resulted in mineralogical and textural modification within (leuco) monzogranitic rocks of the …

The occurrence of ca. 360 Ma greisen-related molybdenite mineralization in the Clayton Hill
biotite–muscovite leucomonzongranite (< 1 km 2) is unusual for the southwestern Meguma …

Granitic rocks in the New Ross area, Nova Scotia, host polymetallic (Cu, Mo, Mn, Sn, U, W),
aplite–pegmatite, greisen, and vein-type mineral deposits. The host granitic rocks belong to …

Abstract Sulfide minerals (Po+ Py+ Ccp>> Sp+ Gn+ Apy) are common constituents of the
Meguma Supergroup (MSG) country rocks, and are also common in the marginal facies of …

The 370 Ma peraluminous South Mountain Batholith (SMB) intrudes Meguma Supergroup
metasedimentary rocks in Nova Scotia. The New Ross area of the SMB contains …