Detrital zircon evidence of Laurentian crustal dominance in the lower Pennsylvanian deposits of the Alleghanian clastic wedge in eastern North America

The late Paleozoic Alleghanian orogeny culminated with the continent–continent collision between Laurentia and Gondwana in the construction of the supercontinent Pangea. Within the Appalachian basin, the sedimentological record of the early stages of the continental collision is preserved as late Mi...

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Veröffentlicht in:	Sedimentary geology 2005-12, Vol.182 (1), p.59-86
Hauptverfasser:	Becker, Thomas P., Thomas, William A., Samson, Scott D., Gehrels, George E.
Format:	Artikel
Sprache:	eng
Schlagworte:	Alleghanian Appalachian basin Detrital zircon Geochronology Pennsylvanian
Online-Zugang:	Volltext
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