Adam S. Chumley scite author profile

Adam S. Chumley

5Publications

1Citation Statement Received

0Citation Statements Given

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University of Northern Colorado

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Paleoproterozoic tectonics of the northern Colorado Rocky Mountains Front Range, USA

Baird

Grover

Mahan

et al. 2022

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SUPPLEMENTAL MATERIAL Methods Sensitive High Resolution Ion Microprobe-Reverse Geometry (SHRIMP-RG) zircon U-Pb sample preparation and analysis by the United States Geological Survey (USGS)The general methods used to obtain zircon U-Pb dates from samples reported in Tables S1, S2, and S6 is as follows. Rock samples were pulverized and sieved to select material sized about 75-600 microns. Density separation via methylene iodide (3.32 g/cm 3 density) and

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Tectonic Style Insights From Paleoproterozoic Amphibolite Geochemistry, Big Thompson and Poudre Canyons, Northern Colorado Front Range

Baird¹,

Chumley²

2022

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Paleoproterozoic Igneous Rocks of the Colorado Front Range as Indicators of Subduction Zone Processes During Basin Closure and Accretion

Hooker¹,

Baird²,

Chumley³

et al. 2019

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Constraining Paleoproterozoic Timing and Settings of Deposition and Tectonism in the Big Thompson and Rist Canyon Areas, Northern Colorado Front Range

Baird¹,

Premo²,

Muller³

et al. 2019

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Geochemistry of the Big Thompson Canyon Paleoproterozoic Granitoids, Northern Colorado Front Range: Implications for Tectonic Activity and Crustal Growth at ~1.7 Ga

Chumley¹,

Baird²,

Kelly³

et al. 2017

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Adam S. Chumley

Paleoproterozoic tectonics of the northern Colorado Rocky Mountains Front Range, USA

Tectonic Style Insights From Paleoproterozoic Amphibolite Geochemistry, Big Thompson and Poudre Canyons, Northern Colorado Front Range

Paleoproterozoic Igneous Rocks of the Colorado Front Range as Indicators of Subduction Zone Processes During Basin Closure and Accretion

Constraining Paleoproterozoic Timing and Settings of Deposition and Tectonism in the Big Thompson and Rist Canyon Areas, Northern Colorado Front Range

Geochemistry of the Big Thompson Canyon Paleoproterozoic Granitoids, Northern Colorado Front Range: Implications for Tectonic Activity and Crustal Growth at ~1.7 Ga

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