[1] Tiepolo M., Tribuzio R., “Slab-melting during Alpine orogeny: evidence from mafic cumulates of the Adamello batholith (Central Alps, Italy)”, Chemical Geology, 216 (2005) 271– 288.
[2] Giacomini F., Tiepolo M., Dallai, L., Ghezzo, C., “On the onset and evolution of the Ross-orogeny magmatism in North Victoria Land- Antarctica, Chemical Geology”, 240 (2007) 103–128.
[3] Molina J.F., Scarrow J.H., Montero P.G., Bea F., “High-Ti amphibole as a petrogenetic indicator of magma chemistry: evidence for mildly alkalic-hybrid melts during evolution of Variscan basic–ultrabasic magmatism of Central Iberia”, Contribution to Mineralogy and Petrology 158 (2009) 69-98.
[4] Götze J., Plötze M., Graupner T., Hallbauer D.K., Bray C.J., “Trace element incorporation into quartz: a combined study by ICP-MS, electron spin resonance, cathodoluminescence, capillary ion analysis, and gas chromatography”, Geochimica and Cosmochimica Acta 68 (2004) 3741–3759.
[5] Larsen R.B., Henderson H., Ihlen P.M., Jacamon F., “Distribution and petrogenetic behaviour of trace elements in granitic pegmatite quartz from granite from South Norway”, Contributions to Mineralogy and Petrology 147 (2004) 615–628.
[6] Jacamon F., Larsen R.B., “Trace element evolution of quartz in the charnockitic Kleivan granite, SW-Norway: The Ge/Ti ratio of quartz as an index of igneous differentiation”, Lithos 107 (2009) 281–291.
[7] مظهری س.ع.، "پتروژنز توده های نفوذی نقده- سردشت"، رساله دکتری، دانشگاه تربیت معلم تهران (1387) 215 صفحه.
[8] Mazhari S.A., Amini S., Ghalamghash J., Bea F., "The origin of mafic rocks in the Naqadeh intrusive complex, Sanandaj-Sirjan Zone, NW Iran, Arabian Journal of Geosciences", (2010) doi: 10.1007/s12517-010-0142-1.
[9] Mazhari S.A., Amini S., Ghalamghash J., Bea F., "Petrogenesis of granitic unit of Naqadeh complex, Sanandaj-Sirjan Zone, NW Iran", Arabian Journal of Geosciences 4 (2011) 59-76.
[10] Alavi M., "Tectonic of the Zagros orogenic belt of Iran: new data and interpretations", Tectonophysics 229 (1994) 211–238.
[11] Alavi M., "Regional stratigraphy of the Zagros fold-thrust belt of Iran and its proforeland evolution”, American Journal of Science 304 (2004) 1-20.
[12] Ahmadi Khalaji A., Esmaeily D., Valizadeh M.V., Rahimpour-Bonab H., "Petrology and geochemistry of the granitoid complex of Boroujerd, Sanandaj-Sirjan Zone, Western Iran", Journal of Asian Earth Sciences 29 (2007) 859-877.
[13] Ghalamghash J., Nedelec A., Bellon H., Vousoughi Abedini M., Bouchez J.L., “The Urumieh plutonic complex (NW Iran): A record of the geodynamic evolution of the Sanandaj–Sirjan zone during Cretaceous times – Part I: Petrogenesis and K/Ar dating”, Journal of Asian Earth Sciences 35 (2009) 401-415.
[14] Bea F., Mazhari A., Montero P., Amini S., Ghalamghash J., “Zircon dating, Sr and Nd isotopes, and element geochemistry of the Khalifan pluton, NW Iran: Evidence for Variscan Magmatism in a supposedly Cimmerian superterrane”, Journal of Asian Earth Sciences 40 (2011) 172-179.
[15] Mazhari S.A., Bea F., Amini S., Ghalamghash J., Molina J.F., Pillar M., Scarrow J.H., Williams S., “The Eocene bimodal Piranshahr massif of the Sanandaj-Sirjan Zone, NW Iran. A marker of the end of the collision in the Zagros Orogen”, Journal of Geological Society 166 (2009) 53-69.
[16] Eftekharnejad J., “(1:250000) geological map of Mahabad”, Geological Survey of Iran Press (1973)
[17] خدابنده ع.ا. ، سلطانی غ. ، "نقشه زمین شناسی 1:100000 نقده"، سازمان زمین شناسی و اکتشافات معدنی کشور (1383)
[18] Halliburton L.E., Jani M.G., Bossoli R.B., “Electron spin resonance and optical studies of oxygen vacancy centers in quartz”, Nuclear Instrumental Methods Physical Research B1 (1984), 192–197.
[19] Nockolds S.R., Allen R.,”The geochemistry of some igneous rock series. Part III”, Geochimica and Cosmochimica Acta 9 (1956) 34–77.
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