Laurentian crustal recycling in the Ordovician Grampian Orogeny: Nd isotopic evidence from Western Ireland

A. E. Draut, Peter Dominic Clift, D. M. Chew, M. J. Cooper, R. N. Taylor, R. E. Hannigan

Research output: Contribution to journalArticle

37 Citations (Scopus)

Abstract

Because magmatism associated with subduction is thought to be the principal source for continental crust generation, assessing the relative contribution of pre-existing (subducted and assimilated) continental material to arc magmatism in accreted arcs is important to understanding the origin of continental crust. We present a detailed Nd isotopic stratigraphy for volcanic and volcaniclastic formations from the South Mayo Trough, an accreted oceanic arc exposed in the western Irish Caledonides. These units span an arc-continent collision event, the Grampian (Taconic) Orogeny, in which an intra-oceanic island arc was accreted onto the passive continental margin of Laurentia starting at similar to 475 Ma (Arenig). The stratigraphy corresponding to pre-, syn- and post-collisional volcanism reveals a progression of epsilon(Nd(t)) from strongly positive values, consistent with melt derivation almost exclusively from oceanic mantle beneath the arc, to strongly negative values, indicating incorporation of continental material into the melt. Using epsilon(Nd(t)) values of meta-sediments that represent the Laurentian passive margin and accretionary prism, we are able to quantify the relative proportions of continent-derived melt at various stages of arc formation and accretion. Mass balance calculations show that mantle-derived magmatism contributes substantially to melt production during all stages of arc-continent collision, never accounting for less than 21 % of the total. This implies that a significant addition of new, rather than recycled, continental crust can accompany arc-continent collision and continental arc magmatism.

Original languageEnglish
Pages (from-to)195-207
Number of pages12
JournalGeological Magazine
Volume141
Issue number2
DOIs
Publication statusPublished - 2004

Keywords

  • Grampian Orogeny
  • western Ireland
  • continental crust
  • Nd isotopes
  • Laurentia
  • Iapetus Ocean
  • ARC-CONTINENT COLLISION
  • CLEW BAY COMPLEX
  • SOUTH MAYO
  • GEOCHEMICAL EVOLUTION
  • U-PB
  • IRISH CALEDONIDES
  • TRACE-ELEMENT
  • ISLAND-ARC
  • SM-ND
  • CONNEMARA

Cite this

Draut, A. E., Clift, P. D., Chew, D. M., Cooper, M. J., Taylor, R. N., & Hannigan, R. E. (2004). Laurentian crustal recycling in the Ordovician Grampian Orogeny: Nd isotopic evidence from Western Ireland. Geological Magazine, 141(2), 195-207. https://doi.org/10.1017/S001675680400891X

Laurentian crustal recycling in the Ordovician Grampian Orogeny: Nd isotopic evidence from Western Ireland. / Draut, A. E.; Clift, Peter Dominic; Chew, D. M.; Cooper, M. J.; Taylor, R. N.; Hannigan, R. E.

In: Geological Magazine, Vol. 141, No. 2, 2004, p. 195-207.

Research output: Contribution to journalArticle

Draut, AE, Clift, PD, Chew, DM, Cooper, MJ, Taylor, RN & Hannigan, RE 2004, 'Laurentian crustal recycling in the Ordovician Grampian Orogeny: Nd isotopic evidence from Western Ireland', Geological Magazine, vol. 141, no. 2, pp. 195-207. https://doi.org/10.1017/S001675680400891X
Draut, A. E. ; Clift, Peter Dominic ; Chew, D. M. ; Cooper, M. J. ; Taylor, R. N. ; Hannigan, R. E. / Laurentian crustal recycling in the Ordovician Grampian Orogeny: Nd isotopic evidence from Western Ireland. In: Geological Magazine. 2004 ; Vol. 141, No. 2. pp. 195-207.
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AU - Draut, A. E.

AU - Clift, Peter Dominic

AU - Chew, D. M.

AU - Cooper, M. J.

AU - Taylor, R. N.

AU - Hannigan, R. E.

PY - 2004

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N2 - Because magmatism associated with subduction is thought to be the principal source for continental crust generation, assessing the relative contribution of pre-existing (subducted and assimilated) continental material to arc magmatism in accreted arcs is important to understanding the origin of continental crust. We present a detailed Nd isotopic stratigraphy for volcanic and volcaniclastic formations from the South Mayo Trough, an accreted oceanic arc exposed in the western Irish Caledonides. These units span an arc-continent collision event, the Grampian (Taconic) Orogeny, in which an intra-oceanic island arc was accreted onto the passive continental margin of Laurentia starting at similar to 475 Ma (Arenig). The stratigraphy corresponding to pre-, syn- and post-collisional volcanism reveals a progression of epsilon(Nd(t)) from strongly positive values, consistent with melt derivation almost exclusively from oceanic mantle beneath the arc, to strongly negative values, indicating incorporation of continental material into the melt. Using epsilon(Nd(t)) values of meta-sediments that represent the Laurentian passive margin and accretionary prism, we are able to quantify the relative proportions of continent-derived melt at various stages of arc formation and accretion. Mass balance calculations show that mantle-derived magmatism contributes substantially to melt production during all stages of arc-continent collision, never accounting for less than 21 % of the total. This implies that a significant addition of new, rather than recycled, continental crust can accompany arc-continent collision and continental arc magmatism.

AB - Because magmatism associated with subduction is thought to be the principal source for continental crust generation, assessing the relative contribution of pre-existing (subducted and assimilated) continental material to arc magmatism in accreted arcs is important to understanding the origin of continental crust. We present a detailed Nd isotopic stratigraphy for volcanic and volcaniclastic formations from the South Mayo Trough, an accreted oceanic arc exposed in the western Irish Caledonides. These units span an arc-continent collision event, the Grampian (Taconic) Orogeny, in which an intra-oceanic island arc was accreted onto the passive continental margin of Laurentia starting at similar to 475 Ma (Arenig). The stratigraphy corresponding to pre-, syn- and post-collisional volcanism reveals a progression of epsilon(Nd(t)) from strongly positive values, consistent with melt derivation almost exclusively from oceanic mantle beneath the arc, to strongly negative values, indicating incorporation of continental material into the melt. Using epsilon(Nd(t)) values of meta-sediments that represent the Laurentian passive margin and accretionary prism, we are able to quantify the relative proportions of continent-derived melt at various stages of arc formation and accretion. Mass balance calculations show that mantle-derived magmatism contributes substantially to melt production during all stages of arc-continent collision, never accounting for less than 21 % of the total. This implies that a significant addition of new, rather than recycled, continental crust can accompany arc-continent collision and continental arc magmatism.

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KW - ARC-CONTINENT COLLISION

KW - CLEW BAY COMPLEX

KW - SOUTH MAYO

KW - GEOCHEMICAL EVOLUTION

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KW - TRACE-ELEMENT

KW - ISLAND-ARC

KW - SM-ND

KW - CONNEMARA

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JO - Geological Magazine

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ER -