2011
DOI: 10.1130/b30503.1
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Detrital zircon geochronology and provenance of the Neoproterozoic to Late Devonian Franklinian Basin, Canadian Arctic Islands

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Cited by 93 publications
(103 citation statements)
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“…Both samples clearly accumulated on the cratonal margin of North America, although the Nation River Formation also received detritus from a peri-cratonic source terrane to the north (Gehrels et al, 1999;Beranek et al, 2010;Anfi nson et al, 2011).…”
Section: Samples Analyzedmentioning
confidence: 97%
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“…Both samples clearly accumulated on the cratonal margin of North America, although the Nation River Formation also received detritus from a peri-cratonic source terrane to the north (Gehrels et al, 1999;Beranek et al, 2010;Anfi nson et al, 2011).…”
Section: Samples Analyzedmentioning
confidence: 97%
“…These samples record infl uence from both the North American craton and the Franklinian orogen to the north (Beranek et al, 2010;Anfi nson et al, 2011).…”
Section: Samples Analyzedmentioning
confidence: 99%
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“…1) . 12), with subordinate older detritus (Anfinson et al 2011;Beranek et al 2013;Hadlari et al 2014). The detrital age spectra from the Franklinian Basin and Peary Land record the detrital signature of autochthonous strata in northern and northeastern Laurentia.…”
Section: Linking the Pearya Terrane With Circum-arctic Terranes And Tmentioning
confidence: 97%
“…Normalized probability density plots comparing the Pearya Terrane sample groups with detrital zircon data sets from autochthonous Laurentian strata and the Arctic Alaska-Chukotka Terrane. Age spectra are from Peary Land (Kirkland et al 2009); the Archer Fiord, Rawlings Bay, and Kennedy Channel Formations in the Franklinian Basin shelf environment (Anfinson et al 2011;Hadlari et al 2014); the Grant Land Formation and Nesmith Beds in the Franklinian Basin deep-water environment (Beranek et al 2013;Hadlari et al 2014); Proterozoic to Cambrian sediments of northwest Laurentia (Hadlari et al 2012); Neoproterozoic to Cambrian strata of the North Slope Subterrane (Macdonald et al 2009;Strauss et al 2013); and Cambrian or younger Group 1 metasediments on the Seward Peninsula (Amato et al 2009) in the Arctic Alaska-Chukotka Terrane. All plots used the same criteria employed for the Pearya Terrane data of this study (see text for discussion).…”
Section: Neoproterozoic Paleogeography Of the Pearya Terranementioning
confidence: 99%