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High Precision Mass Spectrometric Determinations of ^(234)U & ^(230)Th: Application to Quaternary Geology

Chen, J. H. and Wasserburg, G. J. (1988) High Precision Mass Spectrometric Determinations of ^(234)U & ^(230)Th: Application to Quaternary Geology. Chemical Geology, 70 (1-2). p. 173. ISSN 0009-2541. http://resolver.caltech.edu/CaltechAUTHORS:20131028-134157384

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Abstract

Conventionally, the U-series dating methods involve measuring the activity of U and its daughter nuclides. It is well-known that measuring all the nuclides in a sample as compared to counting only the activity can result in a substantial increase in sensitivity (e.g., ^(14)C and ^(10)Be.


Item Type:Article
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URLURL TypeDescription
http://dx.doi.org/10.1016/0009-2541(88)90703-6DOIArticle
http://www.sciencedirect.com/science/article/pii/0009254188907036PublisherArticle
Additional Information:© 1988 Published by Elsevier B.V.
Record Number:CaltechAUTHORS:20131028-134157384
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20131028-134157384
Official Citation:J.H. Chen, G.J. Wasserburg, High precision mass spectrometric determinations of 234U & 230Th: Application to quaternary geology, Chemical Geology, Volume 70, Issues 1–2, 1 August 1988, Page 173, ISSN 0009-2541, http://dx.doi.org/10.1016/0009-2541(88)90703-6. (http://www.sciencedirect.com/science/article/pii/0009254188907036)
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:42098
Collection:CaltechAUTHORS
Deposited By: Ruth Sustaita
Deposited On:28 Oct 2013 21:10
Last Modified:28 Oct 2013 21:10

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