Articles | Volume 2, issue 2
https://doi.org/10.5194/gchron-2-257-2020
https://doi.org/10.5194/gchron-2-257-2020
Research article
 | 
23 Sep 2020
Research article |  | 23 Sep 2020

LA-ICPMS U–Pb geochronology of detrital zircon grains from the Coconino, Moenkopi, and Chinle formations in the Petrified Forest National Park (Arizona)

George Gehrels, Dominique Giesler, Paul Olsen, Dennis Kent, Adam Marsh, William Parker, Cornelia Rasmussen, Roland Mundil, Randall Irmis, John Geissman, and Christopher Lepre

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to revisions (further review by editor and referees) (26 Mar 2020) by Pieter Vermeesch
AR by George Gehrels on behalf of the Authors (28 May 2020)  Author's response   Manuscript 
ED: Publish subject to minor revisions (further review by editor) (05 Jul 2020) by Pieter Vermeesch
AR by George Gehrels on behalf of the Authors (10 Jul 2020)  Author's response   Manuscript 
ED: Publish as is (16 Jul 2020) by Pieter Vermeesch
ED: Publish as is (20 Jul 2020) by Klaus Mezger (Editor)
AR by George Gehrels on behalf of the Authors (31 Jul 2020)  Author's response   Manuscript 
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Short summary
U–Pb ages of zircon crystals are used to determine the provenance and depositional age of strata of the Triassic Chinle and Moenkopi formations and the Permian Coconino Sandstone of northern Arizona. Primary source regions include the Ouachita orogen, local Precambrian basement rocks, and Permian–Triassic magmatic arcs to the south and west. Ages from fine-grained strata provide reliable depositional ages, whereas ages from sandstones are compromised by zircon grains recycled from older strata.