Three billion years of crustal evolution in eastern Canada: Constraints from receiver functions

L. Petrescu (Corresponding Author), I. D. Bastow, F. A. Darbyshire, A. Gilligan, T. Bodin, W. Menke, V. Levin

Research output: Contribution to journalArticle

15 Citations (Scopus)

Abstract

The geological record of SE Canada spans more than 2.5 Ga, making it a natural laboratory for the study of crustal formation and evolution over time. We estimate the crustal thickness, Poisson's ratio, a proxy for bulk crustal composition, and shear velocity (Vs) structure from receiver functions at a network of seismograph stations recently deployed across the Archean Superior Craton, the Proterozoic Grenville, and the Phanerozoic Appalachian provinces. The bulk seismic crustal properties and shear velocity structure reveal a correlation with tectonic provinces of different ages: the post-Archean crust becomes thicker, faster, more heterogeneous, and more compositionally evolved. This secular variation pattern is consistent with a growing consensus that crustal growth efficiency increased at the end of the Archean. A lack of correlation among elevation, Moho topography, and gravity anomalies within the Proterozoic belt is better explained by buoyant mantle support rather than by compositional variations driven by lower crustal metamorphic reactions. A ubiquitous ∼20 km thick high-Vs lower crustal layer is imaged beneath the Proterozoic belt. The strong discontinuity at 20 km may represent the signature of extensional collapse of an orogenic plateau, accommodated by lateral crustal flow. Wide anorthosite massifs inferred to fractionate from a mafic mantle source are abundant in Proterozoic geology and are underlain by high-Vs lower crust and a gradational Moho. Mafic underplating may have provided a source for these intrusions and could have been an important post-Archean process stimulating mafic crustal growth in a vertical sense.
Original languageEnglish
Pages (from-to)788-811
Number of pages24
JournalJournal of Geophysical Research: Solid Earth
Volume121
Issue number2
Early online date9 Feb 2016
DOIs
Publication statusPublished - Feb 2016

Fingerprint

crustal evolution
Canada
Archean
Proterozoic
crusts
Earth mantle
receivers
Seismographs
shear
massifs
anorthosite
secular variations
gravity anomalies
cratons
seismographs
Poisson ratio
Tectonics
Geology
geology
Moho

Keywords

  • Bayesian inversion
  • Canada
  • H-k stacking
  • Precambrian crust
  • cratons
  • receiver functions

Cite this

Three billion years of crustal evolution in eastern Canada : Constraints from receiver functions. / Petrescu, L. (Corresponding Author); Bastow, I. D.; Darbyshire, F. A.; Gilligan, A.; Bodin, T.; Menke, W.; Levin, V.

In: Journal of Geophysical Research: Solid Earth, Vol. 121, No. 2, 02.2016, p. 788-811.

Research output: Contribution to journalArticle

Petrescu, L. ; Bastow, I. D. ; Darbyshire, F. A. ; Gilligan, A. ; Bodin, T. ; Menke, W. ; Levin, V. / Three billion years of crustal evolution in eastern Canada : Constraints from receiver functions. In: Journal of Geophysical Research: Solid Earth. 2016 ; Vol. 121, No. 2. pp. 788-811.
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abstract = "The geological record of SE Canada spans more than 2.5 Ga, making it a natural laboratory for the study of crustal formation and evolution over time. We estimate the crustal thickness, Poisson's ratio, a proxy for bulk crustal composition, and shear velocity (Vs) structure from receiver functions at a network of seismograph stations recently deployed across the Archean Superior Craton, the Proterozoic Grenville, and the Phanerozoic Appalachian provinces. The bulk seismic crustal properties and shear velocity structure reveal a correlation with tectonic provinces of different ages: the post-Archean crust becomes thicker, faster, more heterogeneous, and more compositionally evolved. This secular variation pattern is consistent with a growing consensus that crustal growth efficiency increased at the end of the Archean. A lack of correlation among elevation, Moho topography, and gravity anomalies within the Proterozoic belt is better explained by buoyant mantle support rather than by compositional variations driven by lower crustal metamorphic reactions. A ubiquitous ∼20 km thick high-Vs lower crustal layer is imaged beneath the Proterozoic belt. The strong discontinuity at 20 km may represent the signature of extensional collapse of an orogenic plateau, accommodated by lateral crustal flow. Wide anorthosite massifs inferred to fractionate from a mafic mantle source are abundant in Proterozoic geology and are underlain by high-Vs lower crust and a gradational Moho. Mafic underplating may have provided a source for these intrusions and could have been an important post-Archean process stimulating mafic crustal growth in a vertical sense.",
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AU - Levin, V.

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