موسوی حرمی، ر.، 13۹3. رسوب شناسی. چاپ پانزدهم، انتشارات آستان قدس رضوی، 474 ص.
موسوی حرمی، ر.، محبوبی، الف.، نجفی، م. و رستمی زاده، ق.، 1383. ارزیابی پیوستگی رسوبی و شناسایی عوامل کنترل کننده ریزشوندگی در طول رودخانه در پرچین ـ شرق اسفراین. چکیده مقالات بیست و سومین گردهمایی علوم زمین.
سازمان جغرافیایی کشور، 1381. نقشه زمین‌شناسی ایران سری ۱:250000 ایلام.
شرکت نفت مناطق مرکزی ایران، نقشه زمین‌شناسی تنگ بیجار با مقیاس۱:۱۰0۰۰۰.
سازمان جغرافیای ارتش و نیروهای مسلح، 1378. نقشه‌های توپوگرافی۱:۵۰۰۰۰ چمن، گنجوان و زره.
Bertoldi, W., Ashmore, P., & Tubino, M., 2009. A method for estimating the mean bed load flux in braided rivers. Geomorphology, 103: 330-340.
Blair, T.C., & McPherson, J.G., 1994. Alluvial fans and their natural distinction from rivers based on morphology, hydraulic processes, sedimentary processes, and facies. Journal of Sedimentary Research, 64: 451-490.
Catuneanu, O., Khalifa, M.A., & Wanas, H.A., 2006. Sequence stratigraphy of the Lower Cenomanian Bahariya Formation, Bahariya Oasis, Western Desert, Egypt. Sedimentary Geology, 190: 121-137
Coates, G.F., & Hulse, C.A., 1985. A comparation of four methods of size analysis of fine grained sediments. New Zealand Journal of Geology and Geophysics, 28: 329-380.
Coltortia, M., Pieruccini, P., & Rustioni, M., 2008. The Barga Basin (Tuscany): A record of Plio Pleistocene mountain building of the Northern Apennines, Italy. Quaternary International, 189: 56–70.
Coulthard, T.J., & Van De Wiel, M.J., 2013. Modelling in fluvial geomorphology. In: Shroder, J., (ed.), Treatise in Geomorphology. Academic Press, San Diego. 9: 694-710.
Deynoux, M., Ciner, A., Monod, O., Karabukoglu, M., Manatschal, G., & Tuzcu, S., 2005. Facies architecture and depositional evolution of alluvial fan to fan-delta complexes in the tectonically active Miocene Koprüçay Basin, Isparta Angle, Turkey. Sedimentary Geology, 173: 315-343.
Folk, R.L., 1980.Petrology of Sedimentary Rocks. Hemphill Publishing, Austin, TX, 182 p.
Frings, R.M., 2008. Downstream fining in large sand-bed rivers. Earth Science Reviews, 87:39-60.
Gao, C., Boreham, S., Preece, R.C., Gibbard, P.L., & Briant, R.M., 2007. Fluvial response to rapid climate change during the Devensian (Weichselian) Lateglacial in the River Great Ouse, southern England, UK. Sedimentary Geology, 202: 193–210.
Gupta, N., Atkinson, M.P., & Carling, P.A., 2013. Decadal length changes in the fluvial platform of the river Ganga: bringing a mega river to life with Landsat archives. Remote Sensing Letters, 4 (1): 1–9.
Kosun, E., Poisson, A., Ciner, A., Wernli, R., & Monod, O., 2009. Syn-tectonic sedimentary evolution of the Miocene atallar Basin, southwestern Turkey. Journal of Asian Earth Sciences, 34: 466-479.
Lewis, D.W., & McConchie, D., 1994. Analytical Sedimentology. Chapman & Hall, London, 197 p.
Marren, P.M., McCarthy, T.S., Tooth, S., Brandt, D., Stacey, G.G., Leong, A., & Spottiswoode, B., 2006. A comparison of mud and sand dominated meanders in a downstream coarsening reach of the mixed bedrock-alluvial Klip River, eastern Free State, South Africa. Sedimentary Geology, 190: 213– 26.
Madej, M.A., Sutherland, D.G., Lisle, T.E., & Pryor, B., 2009. Channel responses to varying sediment input: A flume experiment modeled after Redwood Creek, California. Geomorphology, 103: 507-519.
Miall, A.D., 2006. The Geology of Fluvial Deposits: Sedimentary Facies, Basin Analysis, and Petroleum Geology. Springer-Verlag, Berlin. 582 p.
Nelson, P.A., & Seminara, G., 2012. A theoretical framework for the morphodynamics of bedrock channels. Geophysical Research Letters, 39 (L06408): 1-5.
Rice, S.P., 1998. Which tributaries disrupt downstream fining along gravel-bed rivers?. Geomorphology, 22: 39–56.
Rice, S., & Church, M., 1998. Grain size along two gravel-bed rivers: statistical variation, spatial pattern and sedimentary links. Earth Surface Processes and Landforms, 23: 345–363.
Rice, S.P., 1999. The nature and controls of downstream fining within sedimentary links. Journal of Sedimentary Research, 69 (1): 32–39.
Rudra, K., 2014. Changing river courses in the western part of the Ganga–Brahmaputra delta. Geomorphology, 227: 87–100.
Simon, A., & Rinaldi, M., 2013. Incised channels: disturbance, evolution and the role of excess transportcapacity and boundary materials in controlling channel response. In: Shroder, J., (ed.), Treatise on Fluvial Geomorphology. Elsevier, Amsterdam, 574–594 p.
Sklar, L.S., Dietrich, W.E., Foufula, E., Lashermes, B., & Bellugi, D., 2006. Do gravel bed river size distributions record channel network structure. Water Resources Research: 42: W06D18.
Tucker, M.E., 2001. Sedimentary Petrology.3rd edition, Blackwell, Oxford, 260 p.
Uba, C.E., Heubeck, C., & Hulka, C., 2005. Facies analysis and basin architecture of the Neogene Sub-andean synorogenic wedge, southern Bolivia. Sedimentary Geology, 180: 91–123.
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