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1

Robb, L. J. U-Pb ages on single detrital zircon grains from the Witwatersrand Basin: Constraints on the age of sedimentation and on the evolution of granites adjacent to the depository. Johannesburg: University of the Witwatersrand, 1989.

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2

Robb, L. J. U-Pb ages on single detrital zircon grains from the Witwatersrand Basin: Constraints on the age of sedimentation and on the evolution of granites adjacent to the depository. Johannesburg: University of the Witwatersrand, 1989.

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3

Toth, Margo I. Constraints on the formation of the Bitterroot lobe of the Idaho Batholith, Idaho and Montana, from U-Pb zircon geochronology and feldspar Pb isotopic data. Washington, DC: U.S. G.P.O., 1992.

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4

E, Zartman Robert, ed. U-Pb ages of volcanogenic zircon from porcellanite beds in the Vaughn member of the mid-Cretaceous Blackleaf Formation, southwestern Montana. Washington: U.S. G.P.O., 1995.

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5

Kinney, Sean Thomas. Re-evaluating the timescale of rift and post-rift magmatism on the Eastern North American Margin via zircon U-Pb geochronology. [New York, N.Y.?]: [publisher not identified], 2021.

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6

B, Stoeser D., Geological Survey (U.S.), and Saudi Arabia. Deputy Ministry for Mineral Resources, eds. U/PB zircon geochronology of the southern part of the Nabitah mobile belt and Pan-African Continental collision in the Saudi Arabian Shield. [Reston, Va.?]: U.S. Geological Survey, 1985.

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7

U-Pb Formation-age zircon geochronology results for the Brian Head, Bull Rush Peak, Casto Canyon, Cottonwood Mountain, Hatch, and Haycock Mountain quadrangles, Utah. Utah Geological Survey, 2013. http://dx.doi.org/10.34191/ofr-621.

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8

U-Pb detrital zircon geochronology results for the Salt Lake City north quadrangle, Utah. Utah Geological Survey, 2016. http://dx.doi.org/10.34191/ofr-657.

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9

U-Pb Zircon Geochronology Results for the Granite Peak and Granite Peak SE Quadrangles, Utah. Utah Geological Survey, 2009. http://dx.doi.org/10.34191/ofr-546.

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10

U-Pb Zircon Geochronology Results for the Davis Knolls, Faust, Ophir, and Vernon Quadrangles, Utah. Utah Geological Survey, 2013. http://dx.doi.org/10.34191/ofr-608.

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11

U-Pb Detrital zircon geochronology results for the Casto Canyon and Wilson Peak quadrangles, Utah. Utah Geological Survey, 2013. http://dx.doi.org/10.34191/ofr-620.

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12

Nelson, D. R. Compilation of SHIRMP U-Pb zircon geochronology data, 1994 (Record / Geological Survey of Western Australia). Geological Survey of Western Australia, 1995.

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13

U-Pb zircon geochronology results for the Angle, Donkey Flat, Farnsworth Peak, Fort Douglas, Quincy Spring quadrangles, Utah. Utah Geological Survey, 2017. http://dx.doi.org/10.34191/ofr-660.

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14

Winkler, Wilfried, and Albrecht von Quadt, eds. Detrital Mineral U/Pb Age Dating and Geochemistry of Magmatic Products in Basin Sequences. MDPI, 2022. http://dx.doi.org/10.3390/books978-3-0365-4953-8.

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15

U-Pb detrital zircon geochronology result for the Brennan Basin Member of the Duchesne River Formation, Duchesne 30' x 60' quadrangle, Duchesne and Wasatch Counties, Utah. Utah Geological Survey, 2014. http://dx.doi.org/10.34191/ofr-635.

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16

Ellam, Rob. 9. Uranium, thorium, and their daughters. Oxford University Press, 2016. http://dx.doi.org/10.1093/actrade/9780198723622.003.0009.

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All isotopes heavier than 208Pb (lead) are radioactive and many of these have half-lives that are long compared to the age of our Solar System. ‘Uranium, thorium, and their daughters’ describes the natural decay series where radioactive isotopes of uranium and thorium decay by α- and β-emission through several stages until a stable lead isotope is produced. The age of the Solar System and Earth has been established at 4.55 Ga through the isochron approach; U-Pb dating was also used to date the boundary between the Cretaceous and Palaeogene geological periods to 66 Ma, the period associated with a mass extinction on Earth when 70 per cent of living things died out.
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