Tectonic evolution and significance of Silurian Early Devonian hinterland-directed deformation in the internal Humber zone of the southern Quebec Appalachians
S Castonguay, A Tremblay - Canadian Journal of Earth …, 2003 - cdnsciencepub.com
In the southern Quebec Appalachians, the early tectonic history of the Laurentian margin
(Humber zone) comprises foreland-propagating, northwest-directed thrust faulting, nappe
emplacement, and regional prograde metamorphism in response to the obduction of large
ophiolitic nappes during the Taconian orogeny. In the internal Humber zone, this event is
dated at 462±3 Ma (late Middle Ordovician), which is interpreted to represent the timing of
near-peak Taconian metamorphism. Superimposed hinterland-directed structures are …
(Humber zone) comprises foreland-propagating, northwest-directed thrust faulting, nappe
emplacement, and regional prograde metamorphism in response to the obduction of large
ophiolitic nappes during the Taconian orogeny. In the internal Humber zone, this event is
dated at 462±3 Ma (late Middle Ordovician), which is interpreted to represent the timing of
near-peak Taconian metamorphism. Superimposed hinterland-directed structures are …
[引用][C] Erratum: Tectonic evolution and significance of Silurian Early Devonian hinterland-directed deformation in the internal Humber zone of the southern Quebec …
S Castonguay, A Tremblay - Canadian Journal of Earth …, 2003 - cdnsciencepub.com
Erratum: Tectonic evolution and significance of Silurian Early Devonian hinterland-directed
deformation in the internal Humber zone of the southern Quebec Appalachians …
deformation in the internal Humber zone of the southern Quebec Appalachians …
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