“…However, the notion that the effective diffusion dimension is an intrinsic property of a mineral-isotopic system seems unlikely, given that subgrain structures in minerals are demonstrably a function of their thermal and deformational histories. Other researchers have found evidence that a does correspond to the half-grain size for most mineral-isotopic systems (e.g., Farley, 2000;Goodwin and Renne, 1991;Hames and Bowring, 1994;Hess et al, 1993;Hodges and Bowring, 1995;Hodges et al, 1994;Onstott et al, 1991;Reiners andFarley, 1999, 2001;Reiners et al, 2004), but this relationship breaks down in samples subjected to intensive ductile or brittle deformation (e.g., Arnaud and Eide, 2000;Kramar et al, 2001;Mulch et al, 2002). In general, it seems prudent to assume that a is related to the physical grain size when applying eqns [18] and [20] unless samples show textural evidence for the extensive development of subgrain boundaries that may act as fast diffusion pathways, orin the case of K-feldspar -show direct evidence of the existence of multiple diffusion domains during incremental heating experiments.…”