Articles | Volume 2, issue 2
https://doi.org/10.5194/gchron-2-257-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gchron-2-257-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
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
CORRESPONDING AUTHOR
Department of Geosciences, University of Arizona, Tucson, AZ 85721, USA
Dominique Giesler
Department of Geosciences, University of Arizona, Tucson, AZ 85721, USA
Paul Olsen
Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY
10964, USA
Dennis Kent
Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY
10964, USA
Earth and Planetary Sciences, Rutgers University, Piscataway, NJ
08854, USA
Adam Marsh
Petrified Forest National Park, Petrified Forest, AZ 86028, USA
William Parker
Petrified Forest National Park, Petrified Forest, AZ 86028, USA
Cornelia Rasmussen
Berkeley Geochronology Center, 2455 Ridge Rd., Berkeley, CA 94709, USA
Roland Mundil
Berkeley Geochronology Center, 2455 Ridge Rd., Berkeley, CA 94709, USA
Randall Irmis
Natural History Museum of Utah and Department of Geology &
Geophysics, University of Utah, Salt Lake City, UT 84108, USA
John Geissman
Department of Geosciences, University of Texas at Dallas, Richardson,
TX 75080, USA
Christopher Lepre
Earth and Planetary Sciences, Rutgers University, Piscataway, NJ
08854, USA
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Discussed (final revised paper)
Latest update: 23 Nov 2024
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.
U–Pb ages of zircon crystals are used to determine the provenance and depositional age of...