کتابنگاری
سهندی، م. ر.، سرتیپی، ا. ه. و حقفرشی، ا.، 1375- نقشه زمینشناسی 100000/1 سنندج، سازمان زمینشناسی و اکتشافات معدنی کشور.
یاجم، س.، ۱۳۹۶- معمای وجود بلورهای زیرکن‌های بازماندی در توده قلای‌لان؛ نشانه‌هایی از پوسته گندوانایی در سنگ‌هایی با ویژگی‌های ایزوتوپی گوشته‌ای، مجله بلورشناسی و کانی‌شناسی ایران، ۲۵ (۱)، صص 67 تا ۷۸.
References
Alirezaei, S. and Hassanzadeh, J., 2012- Geochemistry and zircon geochronology of the Permian A-type Hasanrobat granite, Sanandaj–Sirjan belt: A new record of the Gondwana break-up in Iran. Lithos, 151, 122- 134.
Azizi, H., Asahara, Y., Mehrabi, B. and Chung, S. L., 2011- Geochronological and geochemical constraints on the petrogenesis of high-K granite from the Suffi abad area, Sanandaj-Sirjan Zone, NW Iran, Chemie der Erde, 71, 363- 376.
Azizi, H., Kazemi, T. and Asahara, Y., 2017- A-type granitoid in Hasansalaran complex, northwestern Iran: Evidence for extensional tectonic regime in northern Gondwana in the Late Paleozoic, Journal of Geodynamics, 108, 56- 72.
Bonin, B., 2007- A-type granites and related rocks: evolution of a concept, problems and prospects, Lithos 97, 1- 29.
Bonin, B., 2008- Death of super-continents and birth of oceans heralded by discrete Atype granite igneous events: the case of the Variscan–Alpine Europe. Journal of Geoscience, 53 (3–4), 237- 252.
Clemens, J. D., Holloway, J. R.and White, A. J. R., 1986- Origin of an Atype granite: experimental constraints, American Mineralogist, 71, 317- 324.
Collins, W. J., Beams, S. D., White, A. J. R. and Chappell, B. W., 1982- Nature and origin of A-type granites with particular reference to southeastern Australia, Contributions to Mineralogy and Petrology 80, 189- 200.
Creaser, R. A., Price, R. C. and Wormald, R. J., 1991- A-type granites revisited: assessment of residual-source model, Geology, 19, 163- 166.
DePaolo, D. J., 1981- Neodymium isotopes in the Colorado Front Range and implications for crust formation and Mantle evolution in the Proterozoic. Nature, 291, 193- 197.
Eby, G. N., 1990- The A-type granitoids: a review of their occurrence and chemical characteristics and speculations on their petrogenesis, Lithos 26, 115- 134.
Eby, G. N., 1992- Chemical subdivision of A-type granitoids: petrogenetic and tectonic implications, Geology, 20, 641- 644.
Eby, G. N., 2011- A-type granites: magma sources and their contribution to the growth of the continental crust, Seventh Hutton Symposium on granites and related rocks, abstract volume, 50- 51.
Frost, B. R., Barnes, C. G., Collins, W. J., Arculus, R. J., Ellis, D. J. and Frost, C. D., 2001- A geochemical classification for granitic rocks, Journal of Petrology, 42, 2033- 2048.
Frost, C. D. and Frost, B. R., 2011- On Ferroan (A-type) Granitoids: their Compositional Variability and Modes of Origin, Journal of Petrology, 52, 39- 53.
Govindaraju, K., Potts, P. J., Webb, P. C. and Watson, J. S., 1994- Report on Whin Sill Dolerite WS-E from England and Pitscurrie micrograbbro PM-S from Scotland: assessment by one hundred and four international laboratories, Geostandards Newsletter, 18, 211- 300.
Honarmand, M., Li, X. H., Nabatian, G. and Neubauer, F., 2017- In-situ zircon U-Pb age and Hf-O isotopic constraints on the origin of the Hasan-Robat A-type granite from Sanandaj–Sirjan zone, Iran: implications for reworking of Cadomian arc igneous rocks, Mineralogy and Petrology, 111(5), 659. DOI: 10.1007/s00710-016-0490-y
Kemp, A. I. S., Hawkesworth, C. J., Foster, G. L., Paterson, B. A., Woodhead, J. D., Hergt, J. M., Gray, C. M. and Whitehouse, M. J., 2007- Magmatic and crustal differentiation history of granitic rocks from Hf–O isotopes in zircon, Science, 315, 980- 983.
King, P. L., White, A. J. R., Chappell, B. W. and Allen, M. C., 1997- Characterization and origin of aluminous A-type granites from the Lachlan Fold Belt South-eastern Australia, Journal of Petrology 38, 371- 391.
Loiselle, M. C. and Wones, D. R., 1979- Characteristics and origin of anorogenic granites, Annual Meetings of the Geological Society of America and Associated Societies, San Diego, California, 11, 468.
Martin, R. F., 2006- A-type granites of crustal origin ultimately result from open-system fenitization-type reactions in an extensional environment, Lithos 91, 125- 136.
Mazhari, S. A., Bea, F., Amini, S., Ghalamghash, J., Molina, J. F., Montero, P., Scarrow, J. H., Williams, I. S., 2009- 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 the Geological Society, 166, 53- 69.
McDonough, W. F. and Sun, S. S., 1995- Composition of the Earth, Chemical Geology 120, 223- 253.
Mohajjel, M. and Fergusson, C. L., 2014- Jurassic to Cenozoic tectonics of the Zagros Orogen in northwesternIran, International Geology Review, 56(3), 263- 287.
Molnar, M., 2006- Tertiary Development of the Zagros Mountains, Geol.186- earth history.
Montero, P. and Bea, F., 1998- Accurate determination of 87Rb/86Sr and 147Sm/144Nd ratios by inductively-coupled-plasma mass spectrometry in isotope geoscience: an alternative to isotope dilution analysis, Analytica Chimica Acta, 358, 227- 233.
Moreno, J. A., Molina, J. F., Bea, F., Abu Anbar, M. and Montero, P., 2016- Th-REE- and Nb-Ta-accessory minerals in post-collisional Ediacaran felsic rocks from the Katerina Ring Complex (S. Sinai, Egypt): An assessment for the fractionation of Y/Nb, Th/Nb, La/Nb and Ce/Pb in highly evolved A-type granites, Lithos, 258- 259, 173- 196.
Moreno, J. A., Molina, J. F., Montero, P., Abu Anbar, M., Scarrow, J. H., Cambeses, A. and Bea, F., 2014- Unraveling sources of A-type magmas in juvenile continental crust: Constraints from compositionally diverse Ediacaran post-collisional granitoids in the Katerina Ring Complex, southern Sinai, Egypt, Lithos, 192-195, 56- 85.
Mouthereau, F., Lacombe, O. and Vergés, J., 2012- Building the Zagros collisional orogen: Timing, strain distribution and the dynamics of Arabia/Eurasia plate convergence, Tectonophysics, 532- 535, 27- 60.
Plank, T., 2005- Constraints from thorium/ lanthanium on sediment recycling at subduction zones and the evolution of the continents, Journal of Petrology 46, 921- 944.
Rudnick, R. L. and Gao, S., 2003- Composition of the continental crust. In: Rudnick, R.L. (Ed.), Treatise on Geochemistry, Elsevier, Oxford, 3, 1- 64.
Schmitt, A. K., Emmermann, R., Trumbull, R. B., Buhn, B. and Henjes-Kunst, F., 2001- Petrogenesis and 40Ar/39Ar geochronology of the Brandberg Complex, Namibia: evidence for a major mantle contribution in metaluminous and peralkaline granites, Journal of Petrology, 41, 207- 1239.
Shafaii Moghadam, H., Li, X. H., Ling, X. X., Stern, R. J, Santos, J. F., Meinhold, G., Ghorbani, G. and Shahabi, Sh., 2015- Petrogenesis and tectonic implications of Late Carboniferous A-type granites and gabbronorites in NW Iran: Geochronological andgeochemical constraints, Lithos 212, 266- 279
Whalen, J. B., Currie, K. L., Chappell, B. W., 1987- A-type granites: geochemical characteristics, discrimination and petrogenesis, Contributions Mineralogy and Petrology, 95, 407- 419.
Wu, F., Sun, D., Li, H., Jahn, B. and Wilde, S., 2002- A-type granites in northeastern China: age and geochemical constraints on their petrogenesis, Chemical Geology, 187, 143- 173.
Yajam, S., Montero, P., Scarrow, J., Ghalamghash, J., Razavi, S. M. H. and Bea, F., 2015- The spatial and compositional evolution of the Late Jurassic Ghorveh-Dehgolan plutons of the Zagros Orogen, Iran: SHRIMP zircon U-Pb and Sr and Nd isotope evidence, Geologica Acta, 13)1(, 25- 43.
)