4.5 Article

Mountains in the shadows of time: Three-dimensional density distribution mapping of U-Pb isotopic data as a visualization aid for geochronological information in concordia diagrams

Journal

GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
Volume 7, Issue -, Pages -

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2005GC001052

Keywords

U-Pb ages; concordia diagrams; SHRIMP; probability density distributions; geochronology : sedimentary geochronology; geochronology : instruments and techniques; geochronology : general or miscellaneous

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[ 1] The salient features of a U-Pb concordia diagram (e.g., Pb-206/U-238 versus Pb-207/U-235 or U-238/Pb-206 versus Pb-207/Pb-206) such as local modes and relative discordance are frequently obscured in diagrams based on large sets of data. Simplifying and plotting the data as univariate ages can aid interpretation, but the discordance filtering of such data is arbitrary. A new approach is proposed where the individual analyses are treated as bivariate normal distributions and their values are summed across an x-y grid to produce a three-dimensional probability distribution. This distribution can then be contoured and color mapped to illustrate features relevant to a concordia line. The mathematical basis for this approach is discussed along with the description of a package using the open-license R statistical package.

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