[1] شهیدی ع. فیروزی ب.، شفیعی ع.، "نقشه 1:100000 زمین شناسی روم"، سازمان زمین شناسی و اکتشاف معدنی کشور ( 1378).
[2] Tirrul R., Bell I.R., Griffis R.J., Camp V.E., "The Sistan suture zone of eastern Iran Geological Society of America Bulletin", V.94 (1983) 134-150.
[3] Babazadeh A.S., Robaszynski F., Courme M.D., "New biostratigraphic data from Cretaceous planktic foraminifera in Sahlabad province", eastern Iran, Lithos, V.40 (2007) 445–454.
[4] Zarrinkoub M.H., Kwan-Nang Pang K.N., Chung S.L., Khatib M.M., Mohammadi S.S., Chiu H.Y., Lee H.Y., "Zircon U-Pb age and geochemical constraints on the origin of the Birjand ophiolite", Sistan suture zone, eastern Iran, Lithos 154 (2012) 392–405.
[5] Zarrikoub M.H., Chung S.L., Chiu H.Y., Mohammadi S.S., Khatib M.M., Lin J.H., "Zircon U-Pb age and geochemical constraints from the northern Sistan suture zone on the neotethyan magmatic and tectonic evolution in eastern Iran", An abstract paper in Turkey Symposium: Tectonic Crossroads:Evolving Orogens of Eurasia – Africa – Arabia (2011).
[6] Brocker M., Fotoohi Rad G. R., Thunissen S., "New time constraints for HP metamorphism and exhumation of mélange rocks from the Sistan suture zone", eastern Iran. An abstract paper in Turkey Symposium: Tectonic Crossroads:Evolving Orogens of Eurasia – Africa – Arabia (2011).
[7] Karipi S., Tsikouras B., Hatzipanagiotou K., Grammatikopoulos T.A., "Petrogenetic significance of spinel-group minerals from the ultramafic rocks of the Iti and Kallidromon ophiolites (Central Greece). Lithos", 99 (2007) 136-149.
[8] Arif M., M. Qasim Jan, "Petrotectonic significance of the chemistry of chromite in the ultramafic mafic complexes of Pakistan", Journal of Asian Earth Sciences., 27 (2006) 628-646.
[9] Dick H.J.B., Bullen T., "Chromian spinel as a petrogenetic indicator in abyssal and alpine-type peridotites and spatially associated lavas", Contributions to Mineralogy and Petrology 86 (1984) 54-76.
[10] Droop G. T. R., "A general equation for estimating Fe+3 concentration in ferromagnesian silicates and oxides from microprobe analyses", using stoichiometric criteria. Mineralogical Magazine 51(1987) 431-435.
[11] Soto J.I., sand Soto V.M., "PTMAFIC: software package for thermometry,barometry and activity calculations in mafic rocks using an IBM compatible computer", Computers and Geosciences 21 (1995) 619–652.
[12] Walker R.T., Gans P., Allen M., Jackson J., Khatib M.M., Marsh N., Saunders A., Zarrinkoub M.H., "Late Cenozoic volcanism and rates of active faulting in eastern Iran", Geophysical Journal International .,177 (2009)783-805.
[13] زرینکوب م.ح.، امینی ص.، آفتابی ع.، کریم پور م.ح.، "کانی شناسی، زمین شیمی، موقعیت ساختمانی و ارایه مدل ژنتیکی برای لیستونیت های خاور ایران"، بلور شناسی و کانی شناسی ایران. سال سیزدهم، شماره 2، پاییز و زمستان، (1384) ص 363-.378
[14] Aftabi A., Zarrinkoub M.H., "Petrogeochemistry of listvenite association in metaophiolites of Sahlabad region, eastern Iran: Implications for possible epigenetic Cu–Au ore exploration in metaophiolites", Lithos, V. 156–159 (2013) 186-203.
[15] Barker A.J., "Introduction to metamorphic textures and microstructures. Chapman and Hall", (1990) 265P.
[16] Shelly D., "Microscopic study of Igneous and Metamorphic rocks", Chapman & Hall, London (1993) 184p.
[17] Vernon R.H., "A practical guide to rock microstructure", Cambridge University Press, 594p (2004).
[18] امینی ص.، زرینکوب م.ح.، درویشزاده ع.، "مطالعه گدازههای بازالتی همراه توالی افیولیتی بیرجند"، مجله علوم دانشگاه تهران. جلد 26، شماره 1، (1379) ص 71 – 91.
[19] Deer W.A., Howie R.A., zussman J., "The Rock Forming Minerals", Second Edition. Longman Asia Ltd, Hong Kong, (1992) 696P.
[20] Morimoto N., "Nomenclature of pyroxenes", Mineralogical Magazine, 52 (1988) 535-550.
[21] Irvine T.N., "Chromian spinel as a petrogenetic indicator, part n. Petrologic applications", Canadian Journal of Earth Sciences, 4 (1967) 71-103.
[22] Conrad W. K., Kay R. W., "Ultramafic and mafic inclusions from Adak Island: Crystallization history and implications for the nature of primary magmas and crustal evolution in the Aleutian arc", Journal of Petrology 25 (1984) 88–125.
[23] Haggerty S. E., "Upper mantle opaque mineral stratigraphy and the genesis of metasomatites and alkali-rich melts", Journal of Geological Society of Australia 14 (1988) 687–699.
[24] Kepezhinskas P. K., Defant M. J., Drummond M. S., "Na metasomatism in the island-arc mantle by slab melt-peridotite interaction: evidence from mantle xenoliths in the North Kamchatka arc", Journal of Petrology 36 (1995)1505–1527.
[25] Arai S., "Characterization of spinel peridotites by olivine-spinel compositional relationships", Review and Interpretation. Chemical Geology 113 (1994)191-204.
[26] Kornprobst J., Ohnenstetter D., Ohnenstetter M., "Na and Cr contents in Cpx from peridotites: a possible discriminant between sub-continental and sub-oceanic mantle", Earth and Planetary Science Letters 53 (1981) 241-254.
[27] Wood B.J., Banno S., "Garnet-orthopyroxene and orthopyroxene-clinopyroxene relationships in simple and complex systems", Contributions to Mineralogy and Petrology., 42 (1973)109-124.
[28] Nimis P., Taylor W. R., "Single clinopyroxene thermobarometry for garnet peridotites Part I.Calibration and testing of a Cr-in-Cpx barometer and an enstatite-in-Cpx thermometer", Contributions to Mineralogy and Petrology 139 (2000) 541-554.
[29] Evans B.W., Frost B.R., "Chrome-spinel in progressive metamorphism: A preliminary analysis", Geochimica et Cosmochimica Acta, v. 39 (1975) 959-972.
[30] Fabriès J., "Spinel-olivine geothermometry in peridotites from ultramafic complexes", Contributions to Mineralogy and Petrology, V. 69 (1979) 329 336.
[31] Ballhaus C., Berry R.F., Green D.H., "High pressure experimental calibration of the olivine- orthopyroxene- spinel oxygen geobarometer: implication for the oxidation state of the upper mantle", Contributions to Mineralogy and Petrology, V. 107 (1991) 27-40.
[32] Kubo K., "Dunite formation processes in highly depleted peridotite: Case study of the Iwandake peridotite", Hokkaido, Japan. Journal of Petrology, V.43 (2002) 423-448.
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