Sedimentologic analysis of cores from the Upper Triassic Chinle Formation and the Lower Permian Cutler Formation, Lisbon Valley, Utah (Q84294): Difference between revisions

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Property / author
 
Property / author: Russell F Dubiel / rank
 
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Property / author: Russell F Dubiel / reference
 
Property / addresses place
 
Property / addresses place: United States of America / rank
 
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Property / addresses place: United States of America / reference
 
Property / addresses place
 
Property / addresses place: Utah / rank
 
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Property / addresses place: Utah / reference
 
Property / content URL
 
Property / content URL: https://pubs.usgs.gov/bul/2000e/report.pdf / rank
 
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Property / content URL: https://pubs.usgs.gov/bul/2000e/report.pdf / reference
 
Property / GDDID
 
Property / GDDID: 5d4f70630b45c76cafa45eae / rank
 
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Property / addresses subject
 
Property / addresses subject: Chemistry of Actinide and Lanthanide Elements / rank
 
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Property / addresses subject: Chemistry of Actinide and Lanthanide Elements / reference
 
Property / addresses subject
 
Property / addresses subject: Sedimentary Processes in Earth's Geology / rank
 
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Property / addresses subject: Sedimentary Processes in Earth's Geology / reference
 
Property / addresses subject
 
Property / addresses subject: Paleoredox and Paleoproductivity Proxies / rank
 
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Property / addresses subject: Paleoredox and Paleoproductivity Proxies / reference
 
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Property / OpenAlex ID: W1531616393 / rank
 
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Latest revision as of 04:17, 12 September 2024

Sedimentologic analysis of cores from the Upper Triassic Chinle Formation and the Lower Permian Cutler Formation, Lisbon Valley, Utah; 1993; B; 2000-E; Dubiel, Russell F.; Brown, Janet L.
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Sedimentologic analysis of cores from the Upper Triassic Chinle Formation and the Lower Permian Cutler Formation, Lisbon Valley, Utah
Sedimentologic analysis of cores from the Upper Triassic Chinle Formation and the Lower Permian Cutler Formation, Lisbon Valley, Utah; 1993; B; 2000-E; Dubiel, Russell F.; Brown, Janet L.

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    OpenAlex ID
    W1531616393
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