Arc-continent collision and the formation of continental crust: A new geochemical and isotopic record from the Ordovician Tyrone Igneous Complex, Ireland
Collisions between oceanic island-arc terranes and passive continental margins are thought to have been important in the formation of continental crust throughout much of Earth's history. Magmatic evolution during this stage of the plate-tectonic cycle is evident in several areas of the Ordovic...
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ftlouisianastuir:oai:repository.lsu.edu:geo_pubs-1450 2024-09-15T18:20:17+00:00 Arc-continent collision and the formation of continental crust: A new geochemical and isotopic record from the Ordovician Tyrone Igneous Complex, Ireland Draut, Amy E. Clift, Peter D. Amato, Jeffrey M. Blusztajn, Jerzy Schouten, Hans 2009-05-01T07:00:00Z application/pdf https://repository.lsu.edu/geo_pubs/451 https://doi.org/10.1144/0016-76492008-102 https://repository.lsu.edu/context/geo_pubs/article/1450/viewcontent/451.pdf unknown LSU Scholarly Repository https://repository.lsu.edu/geo_pubs/451 doi:10.1144/0016-76492008-102 https://repository.lsu.edu/context/geo_pubs/article/1450/viewcontent/451.pdf Faculty Publications text 2009 ftlouisianastuir https://doi.org/10.1144/0016-76492008-102 2024-08-08T04:27:15Z Collisions between oceanic island-arc terranes and passive continental margins are thought to have been important in the formation of continental crust throughout much of Earth's history. Magmatic evolution during this stage of the plate-tectonic cycle is evident in several areas of the Ordovician Grampian-Taconic orogen, as we demonstrate in the first detailed geochemical study of the Tyrone Igneous Complex, Ireland. New U-Pb zircon dating yields ages of 493 2 Ma from a primitive mafic intrusion, indicating intra-oceanic subduction in Tremadoc time, and 475 10 Ma from a light rare earth element (LREE)-enriched tonalite intrusion that incorporated Laurentian continental material by early Arenig time (Early Ordovician, Stage 2) during arc-continent collision. Notably, LREE enrichment in volcanism and silicic intrusions of the Tyrone Igneous Complex exceeds that of average Dalradian (Laurentian) continental material that would have been thrust under the colliding forearc and potentially recycled into arc magmatism. This implies that crystal fractionation, in addition to magmatic mixing and assimilation, was important to the formation of new crust in the Grampian-Taconic orogeny. Because similar super-enrichment of orogenic melts occurred elsewhere in the Caledonides in the British Isles and Newfoundland, the addition of new, highly enriched melt to this accreted arc terrane was apparently widespread spatially and temporally. Such super-enrichment of magmatism, especially if accompanied by loss of corresponding lower crustal residues, supports the theory that arc-continent collision plays an important role in altering bulk crustal composition toward typical values for ancient continental crust. © 2009 Geological Society of London. Text Newfoundland LSU Digital Commons (Louisiana State University) Journal of the Geological Society 166 3 485 500 |
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LSU Digital Commons (Louisiana State University) |
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Collisions between oceanic island-arc terranes and passive continental margins are thought to have been important in the formation of continental crust throughout much of Earth's history. Magmatic evolution during this stage of the plate-tectonic cycle is evident in several areas of the Ordovician Grampian-Taconic orogen, as we demonstrate in the first detailed geochemical study of the Tyrone Igneous Complex, Ireland. New U-Pb zircon dating yields ages of 493 2 Ma from a primitive mafic intrusion, indicating intra-oceanic subduction in Tremadoc time, and 475 10 Ma from a light rare earth element (LREE)-enriched tonalite intrusion that incorporated Laurentian continental material by early Arenig time (Early Ordovician, Stage 2) during arc-continent collision. Notably, LREE enrichment in volcanism and silicic intrusions of the Tyrone Igneous Complex exceeds that of average Dalradian (Laurentian) continental material that would have been thrust under the colliding forearc and potentially recycled into arc magmatism. This implies that crystal fractionation, in addition to magmatic mixing and assimilation, was important to the formation of new crust in the Grampian-Taconic orogeny. Because similar super-enrichment of orogenic melts occurred elsewhere in the Caledonides in the British Isles and Newfoundland, the addition of new, highly enriched melt to this accreted arc terrane was apparently widespread spatially and temporally. Such super-enrichment of magmatism, especially if accompanied by loss of corresponding lower crustal residues, supports the theory that arc-continent collision plays an important role in altering bulk crustal composition toward typical values for ancient continental crust. © 2009 Geological Society of London. |
format |
Text |
author |
Draut, Amy E. Clift, Peter D. Amato, Jeffrey M. Blusztajn, Jerzy Schouten, Hans |
spellingShingle |
Draut, Amy E. Clift, Peter D. Amato, Jeffrey M. Blusztajn, Jerzy Schouten, Hans Arc-continent collision and the formation of continental crust: A new geochemical and isotopic record from the Ordovician Tyrone Igneous Complex, Ireland |
author_facet |
Draut, Amy E. Clift, Peter D. Amato, Jeffrey M. Blusztajn, Jerzy Schouten, Hans |
author_sort |
Draut, Amy E. |
title |
Arc-continent collision and the formation of continental crust: A new geochemical and isotopic record from the Ordovician Tyrone Igneous Complex, Ireland |
title_short |
Arc-continent collision and the formation of continental crust: A new geochemical and isotopic record from the Ordovician Tyrone Igneous Complex, Ireland |
title_full |
Arc-continent collision and the formation of continental crust: A new geochemical and isotopic record from the Ordovician Tyrone Igneous Complex, Ireland |
title_fullStr |
Arc-continent collision and the formation of continental crust: A new geochemical and isotopic record from the Ordovician Tyrone Igneous Complex, Ireland |
title_full_unstemmed |
Arc-continent collision and the formation of continental crust: A new geochemical and isotopic record from the Ordovician Tyrone Igneous Complex, Ireland |
title_sort |
arc-continent collision and the formation of continental crust: a new geochemical and isotopic record from the ordovician tyrone igneous complex, ireland |
publisher |
LSU Scholarly Repository |
publishDate |
2009 |
url |
https://repository.lsu.edu/geo_pubs/451 https://doi.org/10.1144/0016-76492008-102 https://repository.lsu.edu/context/geo_pubs/article/1450/viewcontent/451.pdf |
genre |
Newfoundland |
genre_facet |
Newfoundland |
op_source |
Faculty Publications |
op_relation |
https://repository.lsu.edu/geo_pubs/451 doi:10.1144/0016-76492008-102 https://repository.lsu.edu/context/geo_pubs/article/1450/viewcontent/451.pdf |
op_doi |
https://doi.org/10.1144/0016-76492008-102 |
container_title |
Journal of the Geological Society |
container_volume |
166 |
container_issue |
3 |
container_start_page |
485 |
op_container_end_page |
500 |
_version_ |
1810458653027729408 |