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Isotopic composition and distribution of lead, uranium, and thorium in a Precambrian granite

Tilton, George R. and Patterson, Clair and Brown, Harrison and Inghram, Mark and Hayden, Richard and Hess, David and Larsen, Esper, Jr. (1955) Isotopic composition and distribution of lead, uranium, and thorium in a Precambrian granite. Geological Society of America Bulletin, 66 (9). pp. 1131-1148. ISSN 0016-7606. doi:10.1130/0016-7606(1955)66[1131:ICADOL]2.0.CO;2.

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The isotopic compositions and concentrations of lead and uranium have been determined in some separated minerals and the composite of a granite from Monmouth township, Haliburton County, Ontario. The chemical and mass spectrometric methods that were used are described. The age of the zircon from the granite is 1050 million years. Much of the lead, uranium, and thorium exists in chemically unstable and presumably interstitial phases of the granite. A comparison of the observed amounts of uranium, thorium, and lead in the various minerals with those amounts that should have been present, had these three elements existed within the minerals as closed systems, shows a non-balance of these elements in every case. It appears that the granite as a whole has closely approximated a closed system since it was formed with respect to uranium and its decay products, but has been an open system with respect to thorium and its decay products. Interpretations concerning the relationship of these data to lead ores are discussed.

Item Type:Article
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URLURL TypeDescription[1131:ICADOL]2.0.CO;2DOIArticle
Additional Information:Copyright © 1955, The Geological Society of America, Inc. Received April 24, 1954.
Issue or Number:9
Record Number:CaltechAUTHORS:20140806-160339776
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Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:48150
Deposited By: George Porter
Deposited On:07 Aug 2014 15:09
Last Modified:10 Nov 2021 18:04

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