An evaluation of crustal assimilation within the Late Devonian South Mountain Batholith, SW Nova Scotia

J.g  Shellnutt, Jaroslav Dostal

Research output: Contribution to journalArticle

5 Citations (Scopus)

Abstract

The Late Devonian South Mountain Batholith (SMB) of southwestern Nova Scotia is the largest batholith in the Appalachian Orogen of Eastern North America and contains economic deposits of U and Sn. The SMB comprises at least 11 individual plutons, which range in composition from granodiorite to biotite monzogranite, leucomonzogranite and leucogranite. Previous studies have suggested that a combination of fractional crystallization, assimilation of Meguma Supergroup country rocks and an influx of magmatic fluids contributed to the chemical evolution of the SMB. The amount of crustal assimilation is estimated to be as high as 33%. MELTS modelling assuming a starting composition of granodiorite with H 2O = 4 wt%, pressure = 4 kbar (∼12 km) and fO 2 = FMQ can reproduce the chemical evolution observed in the SMB. However, some leucogranites likely require an additional component (e.g. hydrothermal fluids) to explain their alkali metal enrichment (e.g. Na, K, Rb). Zircon saturation thermometry estimates indicate the Salmontail Lake and Scrag Lake granodiorite plutons had high minimum initial temperatures of 823 ± 6 °C and 832 ± 2 °C, respectively, which are similar to low zircon-inheritance granitoids. The TiO 2/Al 2O 3 and alkali-lime ratios of the surrounding country rocks and the leucogranites indicate the amount of crustal assimilation is likely to be between 10% and 20%. Our findings suggest the granodiorites of the SMB were likely produced by partial melting of the sub-Meguma Supergroup (e.g. Avalon terrane) lower crust caused by the contemporaneous injection of high temperature mafic to ultramafic magmas.

Original languageEnglish
Pages (from-to)353-365
Number of pages13
JournalGeological Magazine
Volume149
Issue number3
DOIs
Publication statusPublished - 2012 May 1

Fingerprint

batholith
granodiorite
mountain
country rock
pluton
zircon
alkali metal
leucogranite
lake
hydrothermal fluid
fractional crystallization
lower crust
lime
partial melting
assimilation
evaluation
biotite
terrane
saturation
fluid

Keywords

  • Appalachian Terrane
  • Late Devonian
  • Meguma Supergroup
  • South Mountain Batholith
  • granite
  • peraluminous

ASJC Scopus subject areas

  • Geology

Cite this

An evaluation of crustal assimilation within the Late Devonian South Mountain Batholith, SW Nova Scotia. /  Shellnutt, J.g; Dostal, Jaroslav.

In: Geological Magazine, Vol. 149, No. 3, 01.05.2012, p. 353-365.

Research output: Contribution to journalArticle

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