Northeastern Section - 48th Annual Meeting (18–20 March 2013)

Paper No. 5
Presentation Time: 8:00 AM-12:00 PM

ACADIAN OROGENESIS IN CENTRAL NEWFOUNDLAND


VALVERDE-VAQUERO, Pablo, Instituto Geológico y Minero de España (IGME), La Calera 1, Tres Cantos (Madrid), 28760, Spain, VAN STAAL, Cees R., Geological Survey of Canada, 625 Robson Street, Vancouver, BC V6B 5J3, Canada, DUNNING, Greg, Department of Earth Sciences, Memorial University of Newfoundland (MUN), St. John's, NF A1B 3X5, Canada and MCNICOLL, V., Geol Survey of Canada, 601 Booth Street, Ottawa, ON K1A 0E8, Canada, p.valverde@igme.es

Early Devonian orogenic activity (Acadian sensu stricto) in the Newfoundland Appalachians produced significant metamorphism and plutonism in the southern and eastern parts of the Central Mobile Belt (Gander Zone and Exploits Subzone). This is marked by the formation of the Meelpaeg metamorphic nappe. U-Pb and Ar-Ar dating in central Newfoundland have revealed that the Meelpaeg Subzone (Gander+Exploits) was part of the Acadian high-grade infrastructure, while the nearby Mount Cormack metamorphic complex was in the superstructure and escaped Siluro-Devonian overprint. Thus, the Acadian event appears to be the result of the formation of this “hot-nappe” at 420-411 Ma, and its final west-directed thrusting at ca. 404-400 Ma.