Lu-Hf and Sm-Nd dating of metamorphic garnet: evidence for multiple accretion events during the Caledonian orogeny in Scotland. / Bird, Anna F.; Thirlwall, Matthew F.; Strachan, Rob A.; Manning, Christina J.

In: Journal of the Geological Society, Vol. 170, No. 2, 03.2013, p. 301-317.

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Lu-Hf and Sm-Nd dating of metamorphic garnet: evidence for multiple accretion events during the Caledonian orogeny in Scotland. / Bird, Anna F.; Thirlwall, Matthew F.; Strachan, Rob A.; Manning, Christina J.

In: Journal of the Geological Society, Vol. 170, No. 2, 03.2013, p. 301-317.

Research output: Contribution to journalArticle

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@article{13b461ac79304d15970e84377d6a6d2a,
title = "Lu-Hf and Sm-Nd dating of metamorphic garnet: evidence for multiple accretion events during the Caledonian orogeny in Scotland",
abstract = "Caledonian orogenesis in Scotland is currently interpreted in terms of a Mid-Ordovician arc-continent collision (Grampian event) followed by the Silurian collision of Laurentia with Baltica (Scandian event). Lu-Hf and Sm-Nd garnet ages of c. 475-460 Ma obtained from prograde garnets in metasedimentary successions and metabasic intrusions within the Northern Highland and Grampian terranes confirm that the Mid-Ordovician Grampian orogenic event was approximately synchronous in both terranes. Lu-Hf and Sm-Nd ages of c. 450 Ma obtained from prograde garnets within the Moine nappe of the Northern Highland terrane provide evidence for a hitherto unrecognised Late Ordovician regional metamorphic event. The existing two-stage Grampian-Scandian model for Caledonian orogenesis in northern Scotland is thus overly-simplistic, and the new ages imply a more complex structural evolution. The restriction of the Late Ordovician and Silurian events to the Northern Highland terrane reinforces the suggestion that it was far removed from the Grampian terrane until juxtaposition following major end-Caledonian (Devonian) sinistral displacement along the Great Glen Fault. A similar record of Mid- and Late Ordovician metamorphic events within the Laurentian-derived Uppermost Allochthons of Norway has been attributed to episodic accretion significantly prior to Silurian continent-continent collision and closure of the Iapetus Ocean. ",
author = "Bird, {Anna F.} and Thirlwall, {Matthew F.} and Strachan, {Rob A.} and Manning, {Christina J.}",
year = "2013",
month = mar,
doi = "10.1144/jgs2012-083",
language = "English",
volume = "170",
pages = "301--317",
journal = "Journal of the Geological Society",
issn = "0016-7649",
publisher = "Geological Society of London",
number = "2",

}

RIS

TY - JOUR

T1 - Lu-Hf and Sm-Nd dating of metamorphic garnet: evidence for multiple accretion events during the Caledonian orogeny in Scotland

AU - Bird, Anna F.

AU - Thirlwall, Matthew F.

AU - Strachan, Rob A.

AU - Manning, Christina J.

PY - 2013/3

Y1 - 2013/3

N2 - Caledonian orogenesis in Scotland is currently interpreted in terms of a Mid-Ordovician arc-continent collision (Grampian event) followed by the Silurian collision of Laurentia with Baltica (Scandian event). Lu-Hf and Sm-Nd garnet ages of c. 475-460 Ma obtained from prograde garnets in metasedimentary successions and metabasic intrusions within the Northern Highland and Grampian terranes confirm that the Mid-Ordovician Grampian orogenic event was approximately synchronous in both terranes. Lu-Hf and Sm-Nd ages of c. 450 Ma obtained from prograde garnets within the Moine nappe of the Northern Highland terrane provide evidence for a hitherto unrecognised Late Ordovician regional metamorphic event. The existing two-stage Grampian-Scandian model for Caledonian orogenesis in northern Scotland is thus overly-simplistic, and the new ages imply a more complex structural evolution. The restriction of the Late Ordovician and Silurian events to the Northern Highland terrane reinforces the suggestion that it was far removed from the Grampian terrane until juxtaposition following major end-Caledonian (Devonian) sinistral displacement along the Great Glen Fault. A similar record of Mid- and Late Ordovician metamorphic events within the Laurentian-derived Uppermost Allochthons of Norway has been attributed to episodic accretion significantly prior to Silurian continent-continent collision and closure of the Iapetus Ocean.

AB - Caledonian orogenesis in Scotland is currently interpreted in terms of a Mid-Ordovician arc-continent collision (Grampian event) followed by the Silurian collision of Laurentia with Baltica (Scandian event). Lu-Hf and Sm-Nd garnet ages of c. 475-460 Ma obtained from prograde garnets in metasedimentary successions and metabasic intrusions within the Northern Highland and Grampian terranes confirm that the Mid-Ordovician Grampian orogenic event was approximately synchronous in both terranes. Lu-Hf and Sm-Nd ages of c. 450 Ma obtained from prograde garnets within the Moine nappe of the Northern Highland terrane provide evidence for a hitherto unrecognised Late Ordovician regional metamorphic event. The existing two-stage Grampian-Scandian model for Caledonian orogenesis in northern Scotland is thus overly-simplistic, and the new ages imply a more complex structural evolution. The restriction of the Late Ordovician and Silurian events to the Northern Highland terrane reinforces the suggestion that it was far removed from the Grampian terrane until juxtaposition following major end-Caledonian (Devonian) sinistral displacement along the Great Glen Fault. A similar record of Mid- and Late Ordovician metamorphic events within the Laurentian-derived Uppermost Allochthons of Norway has been attributed to episodic accretion significantly prior to Silurian continent-continent collision and closure of the Iapetus Ocean.

U2 - 10.1144/jgs2012-083

DO - 10.1144/jgs2012-083

M3 - Article

VL - 170

SP - 301

EP - 317

JO - Journal of the Geological Society

JF - Journal of the Geological Society

SN - 0016-7649

IS - 2

ER -