[1] Naldrett A. J., "Talc-carbonate alteration of some serpentinized ultramafic rocks south of Timmins, Ontario.", Journal of Petrology 7 (1966) 489–499.
[2] Bucher K., Frey M., "Petrogenesis of Metamorphic Rocks.", Springer Verlag, Berlin, Germany (2001).
[3] Hansen L. D., Dipple G. M., Gordon T. M., Kellett D. A., "Carbonated serpentinite (listwanite) at Atlin, British Columbia: a geological analogue to carbon dioxide sequestration.", Canadian Mineralogist 43 (2005) 225–239.
[4] Viti C., Mellini M., "Mesh textures and bastites in the Elba retrograde serpentinites", European Journal of Mineralogy 10 (1998) 1341–1359.
[5] Evans B. W., "The serpentinite multisystem revisited: chrysotile is metastable", International Geological Review 46(2004) 479–506.
[6] Shervais J. W., Kolesar P., Andreasen K., "A field and chemical study of serpentinization —Stonyford, California: chemical flux and mass balance.", International Geological Review 47 (2005) 1–23.
[7] Beinlich A., Austrheim H., Glodny J., Erambert M., Andersen T.B., "CO2 sequestration and extreme Mg depletion in serpentinized peridotite clasts from the Devonian Solund basin, SW Norway.", Geochim Cosmochim Acta 74(24) (2010) 6935–6964.
[8] Snow J. E., Dick H. J. B., "Pervasive magnesium loss by marine weathering of peridotite", Geochim Cosmochim Acta 59 (1995) 4219–4235.
[9] Bulmer C. E., Lavkulich L. M., "Pedogenic and geochemical processes of ultramafic soils along a climatic gradient in southwestern British Columbia.", Canadian Journal of Soil Sciences 74 (1994) 165–177.
[10] Brady P. V., Gislason S. R., "Seafloor weathering controls on atmospheric CO2 and global climate.", Geochim Cosmochim Acta 61 (1997) 965–973.
[11] Cashman S. M., Whetten J. T., "Low-temperature serpentinization of peridotite fanglomerate on the west margin of Chiwaukum graben, Washington.", Geological Society of American Bulletin 87 (1976) 1773–1776.
[12] Craw D., Landis C. A., Kelsey P. I., "Authigenic chrysotile formation in the matrix of Quaternary debris flows, northern Southland", New Zealand. Clays and Clay Minerals 35 (1987) 43–52.
[13] Gilg H.A., Boni M., Balassone G., Allen C.R., Banks D., Moore F., "Marblehosted sulfide ores in the Angouran Zn- (Pb-Ag) deposit, NW Iran: interaction of sedimentary brines with a metamorphic core complex.", Mineralium Deposita 41 (2006) 1-16.
[14] خدابنده ع. ا.، ″نقشه زمین شناسی 100000/1 نقده″، سازمان زمین شناسی و اکتشافات معدنی کشور، 1383.
[15] Kretz R., "Symbols for rock-forming minerals", American Mineralogist 68 (1983) 277-279.
[16] Arai S., "Characterization of spinel peridotites by olivine-spinel compositional relationships: review and interpretation", Chemical Geology113 (1994) 191—204.
[17] Barnes S. J., Roeder P.L., "The range of spinel compositions in terrestrial mafic and ultramafic rocks", Journal of Petrology 42, 2279–2302.
[18] Franz L., Wirth R., "Spinel inclusions in olivine of peridotite xenoliths from TUBAF seamount (Bismark Archipelago/Papua New Guinea): evidence for the thermal and tectonic evolution of the oceanic lithosphere", Contributions to Mineralogy and Petrology 140 (2000) 283–295.
[19] Ishii T., Robinson P.T., Maekawa H., Fiske R., "Petrological studies of peridotites from diapiric serpentinite seamounts in the Izu–Ogasawara–Mariana forearc.", Proceedings of the Ocean Drilling Program - Scientific Results 125 (1992) 445–485.
[20] Stevens R. E., "Composition of some chromites of the western hemisphere", American Mineralogist 29 (1944) 1–34.
[21] Irvine T.N., "Chromian spinel as a petrogenetic indicator. Part 2. Petrologic applications", Canadian Journal of Earth Science 4 (1967) 71-103.
[22] Hey M. H., "A new review of the chlorites", Mineralogical Magazine 30 (1954) 277-292.