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Science Paper
Vol. 315, Issue 10, 2015December 01, 2015 EDT

Synaccretionary Sedimentary and Volcanic Rocks in the Ordovician Tetagouche Backarc Basin, New Brunswick, Canada: Evidence for a Transition From Foredeep to Forearc Basin Sedimentation

Reginald A. Wilson, Cees R. van Staal, William C. McClelland,
synaccretionarydetrital zirconPopelogan arcTetagouche backarcMatapedia forearcBrunswick subduction complexBathurst SupergroupFournier SupergroupGanderiaSalinic orogenyturbidites
https://doi.org/10.2475/10.2015.03
American Journal of Science
Wilson, R. A., van Staal, C. R., & McClelland, W. C. (2015). Synaccretionary sedimentary and volcanic rocks in the Ordovician Tetagouche backarc basin, New Brunswick, Canada: Evidence for a transition from foredeep to forearc basin sedimentation. American Journal of Science, 315(10), 958–1001. https:/​/​doi.org/​10.2475/​10.2015.03
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