A new concordia age for the 'forearc' Bay of Islands Ophiolite Complex, Western Newfoundland utilizing spatially-resolved LA-ICP-MS U-Pb analyses of zircon
Author:
Funder
National Science Foundation
Publisher
Elsevier BV
Subject
Geology
Reference146 articles.
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3. Geology and Geochemistry of an Alkali Volcanic Suite (Skinner Cove Formation) in the Humber Arm Allochthon, Newfoundland;Baker,1979
4. Recent Pb loss in zircon: a natural or laboratory - induced phenomenon?;Black;Chem. Geol. Isotope Geosci. Sect.,1987
5. The use of multiple reference samples for the monitoring of ion microprobe performance during zircon 207Pb/206Pb age determinations;Black;Geostand. Geoanal. Res.,2005
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2. Synchronous formation of the ‘forearc’ Bay of Islands ophiolite and its basal high-temperature metamorphic sole constrained by U–Pb zircon ages;Geoscience Frontiers;2023-11
3. Geochemistry and geochronology of the Bay of Islands metamorphic sole, Newfoundland, Canada: Protoliths and implications for subduction initiation;GSA Bulletin;2023-04-17
4. Lithium isotopic and fluid mobile trace element systematics of the Bay of Islands altered forearc upper to lower ophiolitic crust;Chemical Geology;2023-04
5. A review and tectonic interpretation of the Taconian–Grampian tract between Newfoundland and Scotland: diachronous accretion of an extensive forearc–arc–backarc system to a hyperextended Laurentian margin and subsequent subduction polarity reversal;Geological Society, London, Special Publications;2023-02-22
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