Maximum depositional age and provenance of the Uinta Mountain Group and Big Cottonwood Formation, northern Utah: Paleogeography of rifting western Laurentia
U-Pb detrital zircon analyses provide a new maximum depositional age constraint on the Uinta Mountain Group (UMG) and correlative Big Cottonwood Formation (BCF) of Utah, and significantly enhance our insights on the mid-Neoproterozoic paleogeographic and
Published in: | Geological Society of America Bulletin |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Association of Engineering Geologists
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Subjects: | |
Online Access: | http://hdl.handle.net/1885/50819 https://doi.org/10.1130/B30094.1 https://openresearch-repository.anu.edu.au/bitstream/1885/50819/5/u4027924xPUB211_2010.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/50819/7/01_Dehler_Maximum_depositional_age_and_2010.pdf.jpg |
Summary: | U-Pb detrital zircon analyses provide a new maximum depositional age constraint on the Uinta Mountain Group (UMG) and correlative Big Cottonwood Formation (BCF) of Utah, and significantly enhance our insights on the mid-Neoproterozoic paleogeographic and |
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