Detrital zircon populations of the eastern Laurentian margin in the Appalachians

Newly compiled U-Pb detrital zircon data from eight geographic domains along the eastern Laurentian margin from Newfoundland (Canada) to Alabama (United States) show a highly consistent signature along strike, with only minor local variations. The Precambrian signature is characterized by a small ca. 2.7 Ga population and a major ca. 1.9-0.9 Ga population that peaks at ca. 1.2-1.0 Ga. Detrital zircon populations are from Laurentian Archean crust (ca. 2.7 Ga population), Paleoproterozoic orogens (ca. 1.9-1.6 Ga), the Granite-Rhyolite Province (ca. 1.5-1.4 Ga), and the Elzevir terrane and Grenville Province (ca. 1.3-0.9 Ga). The Mesoproterozoic populations vary in size depending on proximity to the ca. 1.5-1.4 Ga Granite-Rhyolite Province, the ca. 1245-1225 Ma Elzevir terrane, and the ca. 1.2-0.9 Ga Grenville Province. A middle Ordovician zircon population varies in size along strike depending on input from the Taconic orogenic belt, but it is strongest in the northern Appalachians. Because of the general along-strike consistency in detrital zircon age populations, the compilation of all 7534 concordant U-Pb detrital zircon data can be used in future U-Pb detrital zircon studies as an indicator for eastern Laurentian margin sources.

Automated summary

The newly compiled U-Pb detrital zircon data from eight geographic domains along the eastern Laurentian margin show a consistent signature along strike, with a small ca. 2.7 Ga population and a major ca. 1.9-0.9 Ga population. The different populations of detrital zircon come from various sources including Archean crust, Paleoproterozoic orogens, Granite-Rhyolite Province, Elzevir terrane, and Grenville Province.