B‐Type Olivine Fabrics Within the Cumulate Buck Creek Ultramafic Body Emplaced During Southern Appalachian Taconic Subduction

Abstract The Buck Creek ultramafic complex is a fragment of oceanic cumulate emplaced into the lower Laurentian continental crust during Ordovician Taconic subduction. We document olivine fabrics in the relatively pristine dunites preserved from peak metamorphic conditions of ∼850°C and 1.0–1.4 GPa...

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Bibliographic Details
Main Authors: Virginia L. Peterson, Jeffrey M. Rahl, Samuel DeYoung, Davis Eyth, Madeline Mennenga, Benjamin A. Pummell
Format: Article
Language:English
Published: Wiley 2025-05-01
Series:Geochemistry, Geophysics, Geosystems
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Online Access:https://doi.org/10.1029/2024GC011913
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