No Exploits back-arc basin in the Iapetus suture zone of Ireland
Brian McConnell
Matthew Parkes
Quentin Crowley
Adrian Rushton
10.6084/m9.figshare.3454049.v1
https://geolsoc.figshare.com/articles/dataset/No_Exploits_back-arc_basin_in_the_Iapetus_suture_zone_of_Ireland/3454049
<p>A controversial aspect of the closure history of the Iapetus Ocean concerns the existence of the Exploits basin in Ireland
and Britain. The Exploits–Tetagouche back-arc basin of the Canadian Appalachians opened during the Middle Ordovician as the
Popelogan–Victoria volcanic arc migrated northwards from the Ganderian margin. The Bellewstown Terrane, within the Iapetus
suture zone of Ireland, lies between the Ganderian–Avalonian Leinster Terrane and the Laurentian Grangegeeth Terrane. An early
Ordovician ‘Celtic’ shelly fauna is hosted in volcanogenic breccia that we demonstrate is stratigraphically overlain by shales
with no volcanic horizons. The lower 24 m of shale are unfossiliferous, but shale above this stratigraphic level has yielded
a new graptolite fauna consistent with the upper part of the <em>artus</em> Biozone (Darriwilian, <em>c</em>. 464 Ma). U–Pb zircon dating of the volcanic horizon yields an age of <em>c</em>. 474 Ma. The shale, therefore, appears to represent <em>c</em>. 10 myr of deposition and a significant gap in volcanism. This, together with a Sandbian Anglo-Welsh fauna, suggests that
the Bellewstown Terrane remained in a peri-Gondwanan position throughout the Ordovician. Hence, Exploits back-arc basin opening
and Ganderian arc migration did not occur in the Irish sector of Iapetus.
</p>
2016-06-21 11:51:52
Ordovician
Iapetus suture zone
Ma
horizon
Ganderian arc migration
Ireland
Laurentian Grangegeeth Terrane
fauna
Bellewstown Terrane
Iapetus Ocean concerns
shale
Exploit
Geology