[1] پورسلطانی، م. ر. موسوی حرمی، ر.، لاسمی، ی (1386) تفسیر محیط رسوبی سازند کشفرود (باژوسین بالایی- باتونین زیرین)، بر مبنای ایکنوفسیلها د ر شمال خاور ایران، فصلنامه علوم زمین، شماره 65، صفحات 170- 185.
[2] رئوفیان (1393) بررسی ردیفهای رسوبی ژوراسیک میانی تا بالائی در حوضهی ساختاری- رسوبی بینالود بر مبنای مطالعات چینهشناسی، فسیلشناسی (زیای آمونیتی) و محیط رسوبی، پایاننامه دکتری دانشگاه فردوسی مشهد، 419 صفحه.
[3] سرباز ، ن.، محبوبی،ا .، موسوی حرمی، ر.، خانه باد، م (1395) محیط رسوبی و چینهنگاری سکانسی نهشتههای ژوراسیک میانی: مطالعه موردی از برش ناویا در غرب بجنورد، غرب کپهداغ، پژوهـشهای چیـنهنگاری و رسوبشناسی، شماره 65، صفحات 29-46.
[4] سرباز، ن. محبوبی، ا.، موسوی حرمی، ر.، خانه باد، م.، زیر چاپ، برخاستگاه شیلهای سازند کشفرود در برش ناویا (غرب بحنورد) بر اساس دادههای ژئوشیمیایی، فصلنامه علوم زمین.
[5] سهیلی، م.، سهندی، م (1375) نقشهی زمینشناسی سنخواست به مقیاس 1:100000، سازمان زمینشناسی و اکتشافات معدنی کشور.
[6] Adel, I.M., Akarish, B., Amr M. El-Gohary, N )2008( Petrography and geochemistry of Lower Paleozoic sandstones, East Sinai, Egypt: Implications for provenance and tectonic setting, Journal of African Earth Sciences, 52: 43-54.
[7] Alvarez, N. M., Roser, B.P (2007) Geochemistry of black shales from the Lower Cretaceous Paja Formation, Eastern Cordillera, Colombia: Source weathering, provenance, and tectonic setting, Journal of South American Earth Sciences, 23: 271–289.
[8] Basu, A., Young, S., Suttner, L., James, W., Mack, G.H (1975) Re-evalution of the use of undulatory extinction and crystallinity in detrital quartz for provenance interpretation, Journal of Sedimentary Petrology, 45: 873-882.
[9] Batumike, I.L., Cailteux, H., Kumpunzu, A.B (2006) Lithostratigraply, basin devolopoment, base metal deposits and regeional conelathions of the Neoprotrozic Ngoba and Kondelvngu rock Successions, Central Atican. Gondwana Research, 11:432-447.
[10] Bhatia, M.R (1983) Plate tectonics and geochemical composition of sandstones, Geology 91: 611–626.
[11] Dickinson, W.R., Suczek, D.R (1979) Plate tectonics and sandstone compositions. The American Association of Petroleum Geologist Bulletin, 63: 2164-2182.
[12] Fedo, C.M., Young, G.M., Nest, H.W., Hanchar, J.M (1997) Potassicand sodic metasomatism in the Southern Province of the Canadian Shield: evidence from the Paleoproterozoic Serpent Formation, Huronian Supergroup Canada, Precambrian Research, 84: 17–36.
[13] Folk, E (1980) Petrography of Sedimentary Rocks, Hemphill Publishing Company, 182p.
[14] Gazzi, P (1966) Le arenarie del flysh sopracretaceo dell Appennino modenese; Correlazioni con il flysh di Monghidoro,Mineralogica Petrografica Acta 12: 69-97.
[15] Hayeshi, K., Fujisawa, H., Holland, H.D., Ohmoto, H (1997) Geochemistry of 1.9 sedimentary rocks from northeastern Labrador, Canada, Geochimica et Cosmochimica Acta, 61: 4115–4137.
[16] Jafarzadeh, M., Moussavi-Harami, R., Amini, A., Mahboubi, A., Farzaneh, F (2014) Geochemical constrants on the provenance of Oligocene- Miocene siliciclast deposits (Zivah Formation) of NW Iran: implications for the tectonic evolution of the Caucasus, Arabian Journal of Geosciences, 7: 4245- 2463.
[17] Jin, Z., Li, F., Cao, J., Wang, S. & Yu, J (2006) Geochemistry of Daihai Lake sediments, Inner Mongolia, north China: Implications for provenance, sedimentary sorting and catchment weathering, Geomorphology, 80: 147-163.
[18] Khanehbad, M., Moussavi_Harami, R., Mahboubi, A., Nadjafi, A (2012) Geochemistry of Carboniferous Shales of the Sardar Formation, East Central Iran: Implication for Provenance, Paleoclimate and Paleo-oxygenation conditions at a passive continental margin, Geochemistry International, 50: 777-790.
[19] Kroonenberg, S.B (1994) Effects of provenance, sorting and weathering on the geochemistry of fluvial sands from different tectonic and climatic environments. Proceedings of the 29th International Geological Congress, Part A 69-81.
[20] Lee,Y.L (2002) Provenance Derived from the Geochemistry of Late Paleozoic–Early Mesozoic Mudrocks of the Pyeongan Supergroup, Korea, Sedimentary Geology, 149: 219–235.
[21] Madani, M (1977) A study of the sedimentology, stratigraphy and regional geology of the Jurassic rocks of eastern Kopet Dagh (NE Iran). Unpublished Ph.D. thesis, Royal School of Mines, Imperial College, London, 246 p.
[22] Moosavirad, A. M., Janardhana, M. R., Sethumadhav, M.S., Moghadam, M. R., Shankara, M (2011) Geochemistry of lower Jurassic shales of the Shemshak Formation, Kerman Province, Central Iran: Provenance, source weathering and tectonic setting. Chemie der Erde- Geochemistry, 71: 279–288.
[23] Morton, A.C., Hallsworth, C (2007) Stability of detrital heavy minerals during burial diagenesis. Developments in Sedimentology, 58: 215–245.
[24] Nesbitt, H. W., & Young, G. M (1982) Early Proterozoic climates and plate motions inferred from major element chemistry of lutites. Nature, 299, p.715-717.
[25] Nowrouzi, N., Moussavi-Harami, R., Mahboubi, A., Mahmudy Gharaie, M. H., Ghaemi, F (2013) Petrography and geochemistry of Silurian Niur sandstones, Derenjal Mountains, East Central Iran: implications for tectonic setting, provenance and weathering, Arabian Journal of Geosciences, 7: 2793-2813.
[26] Paikaray, S., Banerjee, S., Mukherji, S (2008) Geochemistry of shales from the Paleoproterozoic to Neoproterozoic Vindhyan Supergroup: Implications on provenance, tectonics and geodynamic significance of the Upper Bajocian-Bathonian Kashafrud Formation, NE Iran. Geological Society, London, Special Publication, 312: 205- 218.
[27] Poursoltani, M.R., Moussavi-Harami, R., Gibling, M.R (2007) Jurassic deep-water fans in the Neo-Tethys Ocean: The Kashafrud Formation of the Kopet-Dagh Basin, Iran, Sedimentary Geology, 198: 53–74.
[28] Potter, P. E., Maynard, J. B. Depetris, P. J (2005) Mud and Mudstones, Springer-Verlag Berlin, 297 p.
[29] Roser, B.P., Korsch, R.J (1988) Provenance signatures of sandstone–mudstone suites determined using discriminant function analysis of major-element data, Chemical Geology, 67: 119–139.
[30] Salehi, M. A., Moussavi-Harami, R., Mahboubi, A., Wilmsen, M., Heubeck, Ch (2014) Tectonic and palaeogeographic implications of compositionalvariations within the siliciclastic Ab-Haji Formation (Lower Jurassic,east central Iran), Neues Jahrbuch für Geologie und Paläontologie – Abhandlungenb, 271: 21-48.
[31] Schieber, J (1992) A combined petrographical-geochemical provenance study of the Newland formation, Mid- Proterozoic of Montana, Geological Magazine, 129: 223–237.
[32] Schneider, S., Hornung, J., Hiderer, M., Garzanti, E (2016) Petrography and geochemistry of modern river sediments in an equatorial environment (Rwenzori Mountains and Albertine rift, Uganda) Implications for weathering and provenance, Sedimentary Geology, 336: 106-119.
[33] Suttner, L.J., Dutta, P.K (1986) Alluvial sandstone composition and Palaeoclimate: framework mineralogy, Journal of Sedimentary Petrology, 56: 329-345.
[34] Taheri, J., Fursich, F.T., Wilmsen, M (2009) Stratigraphy, depositional environments and environments and geodynamic significance of the Upper Bajocian-Bathonian Kashafrud Formation, NE Iran. Geological Society, London, Special Publication 312, 205-218.
[35] Taylor, S.R., McLennan, S.M (1985) The Continental Crust: its Composition and Evolution,Blackwell, Oxford 312p.
[36] Thierry, J (2000) Middle Callovian (157–155 Ma). In: Dercourt J, Gaetani M, Vrielynck B, Barrier Biju- Duval B, Brunet MF, Cadet JP, Crasquin S, Sandulescu M (eds) Atlas Peri-Tethys, Palaeogeographical Maps. CCGM/CGMW, Paris, 1–97.
[37] Wang, F., Liu, Cg., Gao, X., Zhang, H (2014) Provenance and paleogeography of the Late Cretaceous Mengyejing Formation, Simao Basin, southeastern Tibetan Plateau:Whole-rock geochemistry, U–Pb geochronology, and Hf isotopic constraints, Sedimentary Geology, 304: 44-58.
[38] Zand-Moghadam, H., Moussavi-Harami, R., Mahboubi, A., Bavi, H (2013) Comparison of tidalites in silicicastic, carbonate, and mixed siicicastic-carbonate System: examples from Cambrian and Devonian deposits of East-Central Iran, ISRN Geology: 1-21.
[39] Zaid, S.M., Gahtani, F.A (2015) Provenance, diagenesis, tectonic setting, and geochemistry of Hawkesbury Sandstone (Middle Triassic), southern Sydney Basin, Australia, Earth Sciences, 24: 72-98.
[40] Zhang, X., Pease,V., Omma, O., Benedictus.A (2015) Provenance of Late Carboniferous to Jurassic sandstones for southernTaimyr, Arctic Russia: A comparison of heavy mineral analysis by optical and QEMSCAN methods, Sedimentary Geology, 329: 166–176.