Description:    The metapelitic schists of the Golpayegan region can be divided into four groups based on their mineral assemblages: (1) garnet-chloritoid schists, (2) garnet schists, (3) garnet-staurolite schists, and (4) staurolite-kyanite schists. Paleozoic pelagic shales experienced progressive metamorphism and polymetamorphism from greenschist to amphibolite facies along the kyanite geotherm. Mylonitic granites are concentrated in the central part of the region more than in other areas, and formed during the dynamic metamorphic phase by activity on the NW-SE striking Varzaneh and Sfajerd faults. The presence of chloritoid in the metapelites demonstrates low-grade metamorphism in the greenschist facies. The textural and chemical zoning of garnets shows three stages of growth and syntectonic formation. With ongoing metamorphism, staurolite appeared, and the rocks reached amphibolite facies, but the degree of metamorphism did not increase past the kyanite zone. Thus, metamorphism of the pelitic sediments occurred at greenschist to lower amphibolite facies. Thermodynamic studies of these rocks indicate that the metapelites in the north Golpayegan region formed at 511–618°C and 0.24–4.1 kbar. Content Type Journal Article Pages 658-675 DOI 10.1134/S086959111207003X Authors S. Karimi, Department of Geology, University of Isfahan, Hezarjerib Ave Postal Code: 81746-73441 Isfahan, Iran S. M. Tabatabaei Manesh, Department of Geology, University of Isfahan, Hezarjerib Ave Postal Code: 81746-73441 Isfahan, Iran H. Safaei, Department of Geology, University of Isfahan, Hezarjerib Ave Postal Code: 81746-73441 Isfahan, Iran M. Sharifi, Department of Geology, University of Isfahan, Hezarjerib Ave Postal Code: 81746-73441 Isfahan, Iran Journal Petrology Online ISSN 1556-2085 Print ISSN 0869-5911 Journal Volume Volume 20 Journal Issue Volume 20, Number 7