posted on 2016-06-21, 11:34authored byStephanie Flude, Alison M. Halton, Simon P. Kelley, Sarah C. Sherlock, James Schwanethal, Camilla M. Wilkinson
<p>New data from a gem-quality feldspar from Itrongay, Madagascar, record naturally occurring <sup>40</sup>Ar/<sup>39</sup>Ar age profiles which can be numerically modelled by invoking a single diffusion mechanism and show that microtexturally simple
crystals are capable of recording complex thermal histories. We present the longest directly measured, naturally produced
<sup>40</sup>Ar*-closure profiles from a single, homogeneous orthoclase feldspar. These data appear to confirm the assumption that laboratory
derived diffusion parameters are valid in nature and over geological timescales. Diffusion domains are defined by crystal
faces and ancient cracks, thus in gem-quality feldspars the diffusion domain size equates to the physical grain size. The
data also illustrate the potential of large, gem-quality feldspars to record detailed thermal histories over tens of millions
of years and such samples should be considered for future studies on the slow cooling of continental crust.
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