P-T paths from anatectic pelites

A relatively simple petrogenetic grid for partial melting of pelitic rocks in the NCKFMASH system is presented based on the assumption that the only H 2O available for melting is through dehydration reactions. The grid include s both discontinuous and continuous Fe-Mg reactions; contours of Fe/(Fe + M g) for continuous reactions define P-T vectors along which continuous melti ng will occur. For biotite-bearing assemblages (garnet+biotite + sillimanit e + K-feldspar + liquid and garnet + biotite + cordierite + K-feldspar + li quid), Fe/(Fe + Mg) contours have negative slopes and melting will occur wi th increasing temperature or pressure. For biotite-absent assemblages (garn et + cordierite + sillimanite + K-feldspar + liquid or garnet + cordierite + orthopyroxene + K-feldspar + liquid) Fe/(Fe + Mg) contours have flat slop es and melting will occur only with increasing pressure. The grid predicts that abundant matrix K-feldspar should only be observed if rocks are heated at P < 3.8 kbar, that abundant retrograde muscovite should only be observe d if rocks are cooled at P > 3.8 kbar, and that generation of late biotite + sillimanite replacing garnet, cordierite, or as selvages around leucosome s should be common in rocks in which melt is not removed. There is also a p redicted field for dehydration melting of staurolite between 5 and 12 kbar. Textures in migmatites from New Hampshire, USA, suggest that prograde dehy dration melting reactions are very nearly completely reversible during cool ing and crystallization in rocks in which melt is not removed. Therefore, m any reaction textures in "low grade" migmatites may represent retrograde ra ther than prograde reactions.