An Z S, Kutzbach J E, Prell W L et al., 2001. Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan Plateau since Late Miocene times. Nature, 411: 62-66.
Ashworth P J, Lewin J, 2012. How do big rivers come to be different? Earth Science Reviews, 114: 84-107.
Blue B, Brierley G J, Yu G A, 2013. Geodiversity in the Yellow River source zone. Journal of Geographical Sciences, 23(5): 775-792.
Brierley G J, Fryirs K, 2000. River styles, a geomorphic approach to catchment characterization: Implications for river rehabilitation in Bega catchment, New South Wales, Australia. Environmental Management, 25: 661-679.
Brierley G J, Fryirs K A, 2005. Geomorphology and River Management: Applications of the River Styles Framework. Oxford, UK: Blackwell Publishing, 398pp.
Corenblit D, Tabacchi E, Steiger J et al., 2007. Reciprocal interactions and adjustments between fluvial landforms and vegetation dynamics in river corridors: A review of complementary approaches. Earth Science Review, 84: 56-86.
Coulthard T J, 2005. Effects of vegetation on braided stream pattern and dynamics. Water Resources Research, 41:W04003, doi: 10.1029/2004WR003201.
Craddock W H, Kirby E, Harkins N W et al., 2010. Rapid fluvial incision along the Yellow River during headward basin integration. Nature Geoscience, 3: 209-213.
Crosato A, Mosselman E, 2009. Simple physics-based predictor for the number of river bars and the transition between meandering and braiding. Water Resources Research, 45(3): W03424.
Davies N S, Gibling M R, 2011. Evolution of fixed-channel alluvial plains in response to Carboniferous vegetation.Nature Geoscience, 4: 629-632, doi: 10.1038/ngeo1237.
Deng X F, Zhang W J, 1992. Evolution of Quaternary glaciers and environment on the eastern side of the Geladandong Peak. Journal of Glaciology and Geocryology, 14(2): 153-160.
Eaton B C, Giles T R, 2008. Assessing the effect of vegetation-related bank strength on channel morphology and stability in gravel-bed streams using numerical models. Earth Surface Processes and Landforms, 34: 712-724, doi: 10.1002/esp.1768.
Eaton B C, Millar R G, Davidson S, 2010. Channel patterns: Braided, anabranching, and single-thread. Geomorphology, 120(3/4): 353-364.
Fotherby L M, 2009. Valley confinement as a factor of braided river pattern for the Platte River. Geomorphology, 103(4): 562-576.
Fryirs K, Brierley G J, 2010. Antecedent controls on river character and behaviour in partly-confined valley settings:Upper Hunter catchment, NSW, Australia. Geomorphology, 117: 106-120.
Fu B, Awata Y, 2007. Displacement and timing of left-lateral faulting in the Kunlun Fault Zone, northern Tibet, inferred from geologic and geomorphic features. Journal of Asian Earth Sciences, 29(2/3): 253-265.
Graf W L, 1978. Fluvial adjustments to the spread of tamarisk in the Colorado Plateau region. Geological Society of America Bulletin, 89: 1491-1501, doi: 10.1130/0016-7606(1978)89<1491:FATTSO>2.0.CO;2.
Gran K, Paola C, 2001. Riparian vegetation controls on braided stream dynamics. Water Resources Research, 37(12): 3275-3283, doi: 10.1029/2000WR000203.
Gregory K J, Gurnell A M, 1988. Vegetation and river channel form and process. In: Viles H A (ed.). Biogeomorphology.Oxford: Basil Blackwell, 11-42.
Guccione M J, Mueller K, Champion J et al., 2002. Stream response to repeated coseismic folding, Tiptonville dome, New Madrid seismic zone. Geomorphology, 43: 313-349.
Gurnell A M, Petts G E, Hannah D M et al., 2001. Riparian vegetation and island formation along the gravel-bed Fiume Tagliamento, Italy. Earth Surface Processes and Landforms, 26: 31-62.
Harkins N, Kirby E, Heimsath A et al., 2007. Transient fluvial incision in the headwaters of the Yellow River, northeastern Tibet, China. Journal of Geophysical Research, 112(F3): 1-21, F03S04.
Hickin E J, 1984. Vegetation and river channel dynamics. Canadian Geographer, 28: 111-126.
Huang H Q, Chang H H, Nanson G C, 2004. Minimum energy as a general form of critical flow and maximum flow efficiency and for explaining variations in river channel pattern. Water Resources Research, 40, W04502, doi: 10.1029/2003WR002539.
Huang H Q, Nanson G, 2007. Why some alluvial rivers develop an anabranching pattern. Water Resources Research, 43, W07441, doi: 10.1029/2006WR005223.
Huang H Q, Nanson G C, 1997. Vegetation and channel variation: A case study of four small streams in southeastern Australia. Geomorphology, 18: 237-249.
Hupp C R, Osterkamp W R, 1996. Riparian vegetation and fluvial geomorphic processes. Geomorphology, 14: 277-295.
Jiao K Q, Shen Y P, 2003. The Quaternary glaciations and glacier properties in the Tanggula Range. Journal of Glaciology and Geocryology, 25(1): 34-42. (in Chinese)
Leopold L B, Wolman M G, 1957. River channel patterns: Braided, meandering and straight. U.S. Geological Survey Professional Paper, 282-B: 39-85.
Lewin J, Ashworth P J, 2013. Defining large river channel patterns: Alluvial exchange and plurality Geomorphology, doi: 10.1016/j.geomorph.2013.02.024. (in press)
Lewin J, Brindle B J, 1977. Confined meanders. In: Gregory K J (ed.). River Channel Changes. Chichester: John Wiley and Sons, 221-233.
Li J J, Fang X M, Ma H Z, 1996. Geomorphological and environmental evolution in the upper reaches of the
Yellow River during the late Cenozoic. Science in China (Series D), 39(4): 380-390.
Li Y L, Wang C S, Wang M et al., 2006. Morphological features of river valleys in the source region of the Yangtze River, north Tibet, and their response to neotectonic movement. Geology in China, 33(2): 374-382. (in Chinese)
Li Z W, Wang Z Y, Pan B Z et al., 2013. Analysis of controls upon channel planform at the First Great Bend of the Upper Yellow River, Qinghai-Tibet Plateau. Journal of Geographical Sciences, 23(5): 833-848.
McDowell P F, 2001. Spatial variations in channel morphology at segment and reach scales, Middle Fork John Day River, Northeastern Oregon. In: Morava J M, Montgomery D R, Palcsak B B et al. (eds.). Geomorphic Processes and Riverine Habitat. American Geophysical Union, Washington, DC, 159-172.
Micheli E R, Kirchner J W, 2002. Effects of wet meadow riparian vegetation on streambank erosion: 2. Measurements of vegetated bank strength and consequences of failure mechanics. Earth Surface Processes and Landforms, 27: 687-697, doi: 10.1002/esp.340.
Millar R G, 2000. Influence of bank vegetation on alluvial channel patterns. Water Resources Research, 36(4): 1109-1118.
Nanson G C, Huang H Q, 1999. Anabranching rivers: Divided efficiency leading to fluvial diversity. In: Miller A J and Gupta A (eds.), Varieties of Fluvial Form. Chichester: Wiley, 477-494.
Nanson G C, Knighton A D, 1996. Anabranching rivers: Their cause, character and classification. Earth Surf.Processes Landforms, 21: 217-239.
Ouchi S, 1985. Response of alluvial rivers to slow active tectonic movement. Geological Society of America Bulletin, 96: 504-515.
Pan B Z, Wang Z Y, Li Z W et al., 2013. An exploratory analysis of benthic macroinvertebrates as indicators of the ecological status in the Upper Yellow and Yangtze Rivers. Journal of Geographical Sciences, 23(5): 871-882.
Rosgen D L, 1994. A classification of natural rivers. Catena, 22: 169-199.
Rosgen D L, 1996. Applied River Morphology. Wildland Hydrology Books. Colorado: Pagosa Springs, 385pp.
Rust B R, 1978. A classification of alluvial channel systems. In: Miall A D (ed.). Fluvial Sedimentology. Canadian Society of Petroleum Geologists Memoir 5, Calgary, 187-198.
Schumm S A, 1985. Patterns of alluvial rivers. Annual Review of Earth and Planetary Sciences, 13: 5-27.
Schumm S A, Dumont J F, Holbrook J M, 2000. Active Tectonics and Alluvial Rivers. Cambridge: Cambridge University Press, 276pp.
Shi L R, 2001. Rivers and their development processes in the source region of the Yangtze River. Yangtze River Chorography, (3): 95-108. (in Chinese)
Simon A, Collison A J C, 2002. Quantifying the mechanical and hydrologic effects of riparian vegetation on streambank stability. Earth Surface Processes and Landforms, 27: 527-546, doi: 10.1002/esp.325.
Snyder N P, Whipple K X, Tucker G E, Merritts D M, 2003. Channel response to tectonic forcing: analysis of stream morphology and hydrology in the Mendocino triple junction region, northern California. Geomorphology, 53: 97-127.
Spitz W J, Schumm S A, 1997. Tectonic geomorphology of the Mississippi Valley between Osceola, Arkansas and Friars Point, Mississippi. Engineering Geology, 46(3/4): 259-280.
Tal M, Gran K, Murray A B, Paola C et al, 2004. Riparian vegetation as a primary control on channel characteristics in multi-thread rivers. In: Bennett S J and Simon A (eds.). Riparian Vegetation and Fluvial Geomorphology:Hydraulic, Hydrologic, and Geotechnical Interactions. Washington D.C., American Geophysical Union, 43-58.
Tal M, Paola C, 2007. Dynamic single-thread channels maintained by the interactions of flow and vegetation.Geology, 35: 347-350, doi: 10.1130/G23260A.1
Tapponnier P, Xu Z Q, Roger F et al., 2001. Oblique stepwise rise and growth of the Tibet Plateau. Science, 294(5547): 1671-1677.
Wohl E E, 1998. Bedrock channel morphology in relation to erosional processes. In: Tinkler K J, Wohl E E (eds.).Rivers over Rock: Fluvial Processes in Bedrock Channels. Geophysical Monograph Series 107. American Geophysical Union, Washington, 133-152.
Yang J P, Ding Y J, Chen R S, 2006. Spatial and temporal of variations of alpine vegetation cover in the source regions of the Yangtze and Yellow Rivers of the Tibetan Plateau from 1982 to 2001. Environmental Geology, 50: 313-322, doi: 10.1007/s00254-006-0210-8.
Yang T M, 2001. Quaternary glacial remnants in the source region of the Yangtze River. Yangtze River Chorography, (3): 74-78.
Yin A, Harrison T M, 2000. Geologic evolution of the Himalayan-Tibetan orogen. Annual Review of Earth and Planetary Sciences, 28: 211-280.
Zhang L Y, 1981. Glaciers at the source region of Tuotuo River in the upper reaches of the Changjiang and their evolution. Journal of Glaciology and Geocryology, 3(1): 1-9. (in Chinese)
Zheng H X, Zhang X Y, 1988. On tectonics of the Qinghai-Xizang (Tibet) Plateau. Contribution to the Geology of the Qinghai-Xizang (Tibet) Plateau, 19: 73-90. (in Chinese) |