[1] Deer W.A., Howie R.A., Zussman, J., “Epidote group. In: Deer, W.A., Howie, R.A. and Zussman, J. Disilicates and ring silicates”, Longman, Harlow, (1986) 2-179.
[2] Poli S., Schmidt M.W., “The high-pressure stability of zoisite and phase relationships of zoisite-bearing assemblages”, Contributions to Mineralogy and Petrology, 130 (1998) 162-175.
[3] Chatterjee N.D., Johannes W., Leistner H., “The system CaO-Al2O3-SiO2-H2O: new phase equilibria data, some calculated phase relations, and their petrological applications”, Contributions to Mineralogy and Petrology, 88 (1984) 1-13.
[4] Franz G., Selverstone J., “An empirical phase diagram for the clinozoisite-zoisite transformation in the system Ca2Al3Si3O12 (OH)–Ca2Al2Fe3+Si3O12 (OH)”, American Mineralogist, 77 (1992) 631–642.
[5] Jenkins D. M., Newton R. C., Goldsmith J. R., “Fe-free clinozoisite stability relative to zoisite”, Nature, 304 (1983) 622-623.
[6] Holdaway M.J., “Thermal stability of Al -Fe epidote as a function of ƒO2 and Fe content”, Contributions to Mineralogy and Petrology, 37 (1972) 307–340.
[7] Jenkins D. M., Newton R. C., Goldsmith J.R., “Relative Stability of Fe-Free Zoisite and Clinozoisite”, Journal of Geology, 93 (1985) 663-672.
[8] Holland T.J.B., “Stability relations of clino- and orthozoisite”. In: Henderson CMB (ed) Progress in experimental petrology. The Natural Environment Research Council. Publication Series D. 25 (1984) 185–186.
[9] Fehr K.T., Heuss-Aβbichler S., “Intracrystalline equilibria and immiscibility along the join clinozoisite–epidote: an experimental and 57Fe Mossbauer study”, N Jahrb Mineral Abh, 172 (1997) 43–67.
[10] Heuss-Aβbichler S., Fehr K.T., “Intercrystalline exchange of Al and Fe3+ between grossular–andradite and clinozoisite–epidote solid solutions”, N Jahrb Mineral Abh 172 (1997) 69–100
[11] Strens R.G.J., “Stability relations of the Al-Fe epidotes”, Mineral. Mag. 35 (1965) 464-475.
[12] Holdaway M.J., ”Basic regional metamorphic rocks in part of the Klamath Mountains, Northern California”, American Mineralogist 50 (1965) 953-977.
[13] Hietnan A., “Amphibole pairs, epidote minerals, chlorite, and plagioclase in metamorphic rocks, northern Sierra Nevada, California”, American Mineralogist, 59 (1974) 22-40.
[14] Raith M., “The Al-Fe (lll) epidote miscibility gap in a metamorphic profile through the Penninic series of the Tauern Window, Austria”, Contributions to Mineralogy and Petrology, 57 (1976) 99-117.
[15] Brunsmann A., Franz G., Heinrich W., “Experimental investigation of zoisite–clinozoisite phase equilibria in the system CaO–Fe2O3–Al2O3–SiO2–H2O”, Contributions to Mineralogy and Petrology, 143 (2002) 115–130.
[16] Selverstone J., Spear F.S., “Metamorphic P–T paths from pelitic schists and greenstones from the south-west Tauern Window, Eastern Alps”, Journal of metamorphic Geology 3 (1985) 439–465
[17] سازمان زمینشناسی و اکتشافات معدنی کشور، نقشه زمینشناسی 1:100000 سلماس.
[18] سازمان زمینشناسی و اکتشافات معدنی کشور، نقشه زمینشناسی 1:250000 خوی.
[19] Kapp P., Manning C.E., and Tropper P., "Phase-equilibrium constraints on titanite and rutile activities in mafic epidote amphibolites and geobarometry using titanite–rutile equilibria", Journal of metamorphic Geology,. 27 (2009) 509-521.
[20] El-Shazley A.K., Worthing M.A., and Liou J.G., "Interlayered Eclogites, Blueschists and Epidote Amphibolites from NE Oman: a Record of Protolith Compositional Control and Limited Fluid Infiltration", Journal of Petrology, 38 (1997) 1461-1487.
[21] Tsujimori T., Liou J.G., Ernst W.G., Itaya T., "Triassic paragonite- and garnet-bearing epidote-amphibolite from the Hida Mountains, Japan", Gondwana Research,. 9 (2006) 167-175.
[22] Castelli D., Rolfo F., Compagnoni R. and Xu S., "Metamorphic veins with kyanite, zoisite and quartz in the Zhu-Jia-Chong eclogite, Dabie Shan, China", The Island Arc,. 7 (1998) 159-173.
[23] Zack T., Foley S.F., Rivers T., "Equilibrium and disequilibrium trace element partitioning in hydrous eclogites (Trescol,en, Central Alps)", Journal of Petrology, 43 (2002) 1947-1974.
[24] Hacker B.R., A. G.A., Peacock S.M., "Subduction factory 1. Theoretical mineralogy, densities, seismic wave speeds, and H2O contents", Journal of Geophysical Research, 108 (2003) 1-26.
[25] Davis P.B., Whitney D.L., "Petrogenesis of lawsonite and epidote eclogite and blueschist, Sivrihisar Massif, Turkey", Journal of metamorphic Geology,. 24 (2006) 823-849.
[26] Rodgers A. F., “Clinozoisite from Lower California”, American Mineralogist, 9 (1924) 221-224.
[27] Brunsmann A., Franz G., Erzinger J. and Landwehr D., “Zoisite- and clinozoisite-segregations in metabasites (Tauern Window,
Austria) as evidence for high-pressure fluid–rock interaction”,. Journal of metamorphic Geology, 18 (2000) 1–21.
[28] Ackermand D., Raase P., “Coexisting zoisite and clinozoisite in biotite schists from the Hohe Tauern, Austria”, Contributions to Mineralogy and Petrology, 42 (1973) 333-341.
[29] Enami M., Banno S., “Zoisite-clinozoisite relations in low- to medium-grade high-pressure metamorphic rocks and their implications”, Mineralogical Magazine, 43 (1980) 1005-1013.
[30] Prunier A.R., Hewitt D.A., “Experimental observations on coexisting zoisite-clinozoisite”. American Mineralogist, 70 (1985) 375-378.
[31] Dollase W.A., “Refinement of the crystal structures of epidote, allanite and hancockite”, American Mineralogist, 56 (1971) 447-464.
[32] Berman R.G., Brown T.H., “Heat capacity of minerals in the system Na2O–K2O–CaO–MgO–FeO–Fe2O3–Al2O3–SiO2–TiO2–H2O–CO2: representation, estimation, and high temperature extrapolation”, Contribution to Mineralogy and Petrology, 89 (1985) 168–183.
[33] Hemingway B.S., Haas J.L., Robinson G.R., “Thermodynamical properties of selected minerals in the system Al2O3–CaO–SiO2–H2O at 298.15 K and 1 bar (105 Pascal) pressure and at higher temperatures”, Geol Surv Bull 1544 (1982) 1–70.
[34] Spear F. S., “NaSi = CaAl exchange equilibrium between plagioclase and amphibole: An empirical model”, Contrib. Mineral. Petrol., 72 (l980), 33-41.
)