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Our results show that the composition of the detritus and hydrogenous end members may vary significantly between sites within the same basin, challenging the use of a common value representing the contaminating phases.
We thus advocate the independent determination of the end member values for each set of coeval samples and apply these values to the calculation of isochron and single sample ages. before correction) produce ages that are inherently erroneous, the combined 234U-230Th and 235U-231Pa schemes can be used to construct concordia plots that serve as an immediate filter for the validity of data sets and in some cases can be used to directly extract the true age of a given sample set, thus overcoming the necessity to develop complex correction schemes.