File:Thermochronometry.JPG

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There are multiple techniques for capable of providing thermochronometry data in geothermal areas. The U-Pb methods in green determine the ages of high temperature minerals (500-950°C), the 40AR/39AR methods in red have application in medium temperature minerals (150-550°C), and the (U-Th)/He methods cover the low temperature range (40-220°C). http://jdlc.curtin.edu.au/research/geochron.cfm

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current16:16, 28 October 2013Thumbnail for version as of 16:16, 28 October 2013584 × 419 (32 KB)Darren.atkins (Talk | contribs)There are multiple techniques for capable of providing thermochronometry data in geothermal areas. The U-Pb methods in green determine the ages of high temperature minerals (500-950°C), the 40AR/39AR methods in red have application in medium temperat...

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