Natural experiments in landscape evolution
暂无分享,去创建一个
[1] G. Tucker,et al. Investigating the surface process response to fault interaction and linkage using a numerical modelling approach , 2006 .
[2] G. Tucker,et al. Landscape response to tectonic forcing: Digital elevation model analysis of stream profiles in the Mendocino triple junction region, northern California , 2000 .
[3] S. Bonnet,et al. Macroscale dynamics of experimental landscapes , 2006, Geological Society, London, Special Publications.
[4] Mike Kirkby,et al. Some factors controlling gully growth in fine-grained sediments: a model applied in southeast Spain. , 2000 .
[5] W. Dietrich,et al. A mechanistic model for river incision into bedrock by saltating bed load , 2004 .
[6] Rudy Slingerland,et al. Mathematical Modeling of Graded River Profiles , 1987, The Journal of Geology.
[7] Jérôme Lavé,et al. Active folding of fluvial terraces across the Siwaliks Hills, Himalayas of central Nepal , 2000 .
[8] K. Whipple,et al. Knickpoint initiation and distribution within fluvial networks: 236 waterfalls in the Waipaoa River, North Island, New Zealand , 2006 .
[9] Frank J. Pazzaglia,et al. Quantitative testing of bedrock incision models for the Clearwater River, NW Washington State , 2003 .
[10] David R. Montgomery,et al. A process-based model for colluvial soil depth and shallow landsliding using digital elevation data , 1995 .
[11] Gregory E. Tucker,et al. Modeling fluvial incision and transient landscape evolution: Influence of dynamic channel adjustment , 2008 .
[12] W. Dietrich,et al. The soil production function and landscape equilibrium , 1997, Nature.
[13] R. Bras,et al. Numerical modeling of non-steady-state river profile evolution using a sediment-flux-dependent incision model , 2006 .
[14] G. Tucker,et al. Contrasting transient and steady‐state rivers crossing active normal faults: new field observations from the Central Apennines, Italy , 2007 .
[15] E. Kirby,et al. Transient channel incision along Bolinas Ridge, California: Evidence for differential rock uplift adjacent to the San Andreas fault , 2007 .
[16] D. Bourlès,et al. Long-term fluvial incision rates and postglacial river relaxation time in the French Western Alps from 10Be dating of alluvial terraces with assessment of inheritance, soil development and wind ablation effects , 2003 .
[17] Peter K. Haff,et al. Microtopography as an indicator of modern hillslope diffusivity in arid terrain , 1997 .
[18] J. T. Hack. Interpretation of erosional topography in humid temperate regions. , 1960 .
[19] Mike Kirkby,et al. Modelling the links between vegetation and landforms , 1995 .
[20] A. Michetti,et al. Spatial and temporal variations in growth rates along active normal fault systems: an example from The Lazio–Abruzzo Apennines, central Italy , 2004 .
[21] Arjun M. Heimsath,et al. Transient fluvial incision in the headwaters of the Yellow River, northeastern Tibet, China , 2007 .
[22] K. Whipple,et al. Formation of fluvial hanging valleys: Theory and simulation , 2007 .
[23] Kelin X. Whipple,et al. Rates and processes of bedrock incision by the Upper Ukak River since the 1912 Novarupta ash flow in the Valley of Ten Thousand Smokes, Alaska , 2000 .
[24] I. Rodríguez‐Iturbe,et al. A coupled channel network growth and hillslope evolution model: 1. Theory , 1991 .
[25] Robert S. Anderson,et al. Hillslope and channel evolution in a marine terraced landscape , 1994 .
[26] William E. Dietrich,et al. The Problem of Channel Erosion into Bedrock , 1992 .
[27] William E. Dietrich,et al. Modeling fluvial erosion on regional to continental scales , 1994 .
[28] J. Avouac,et al. Investigation of the relationships between basin morphology, tectonic uplift, and denudation from the study of an active fold belt in the Siwalik Hills, central Nepal , 1999 .
[29] G. Tucker,et al. Modelling landscape evolution , 2010 .
[30] W. Dietrich,et al. Longitudinal Profile Development into Bedrock: An Analysis of Hawaiian Channels , 1994, The Journal of Geology.
[31] G. Hancock,et al. Use of a landscape simulator in the validation of the SIBERIA Catchment Evolution Model: Declining equilibrium landforms , 2001 .
[32] K. Whipple,et al. Quantifying differential rock-uplift rates via stream profile analysis , 2001 .
[33] D. Merritts,et al. Bedrock Fluvial Incision and Longitudinal Profile Development Over Geologic Time Scales Determined by Fluvial Terraces , 2013 .
[34] George E. Hilley,et al. Geomorphic response to uplift along the Dragon's Back pressure ridge, Carrizo Plain, California , 2008 .
[35] D. Nash,et al. Forms of bluffs degraded for different lengths of time in emmet county, Michigan, U.S.A. , 1980 .
[36] D. Granger,et al. Dynamic equilibrium among erosion, river incision, and coastal uplift in the northern and central Apennines, Italy , 2008 .
[37] E. Kirby,et al. Tectonic and lithologic controls on bedrock channel profiles and processes in coastal California , 2004 .
[38] Tom J. Coulthard,et al. Landscape evolution models: a software review , 2001 .
[39] S. Gorelick,et al. Paleoclimatic Signature in Terrestrial Flood Deposits , 1992, Science.
[40] P. Allen,et al. Transient landscapes at fault tips , 2007 .
[41] William E. Dietrich,et al. Evidence for nonlinear, diffusive sediment transport on hillslopes and implications for landscape morphology , 1999 .
[42] D. Lague,et al. Laboratory experiments simulating the geomorphic response to tectonic uplift , 2003 .
[43] P. Davy,et al. A stochastic precipiton model for simulating erosion/sedimentation dynamics , 2001 .
[44] David R. Montgomery,et al. Geologic constraints on bedrock river incision using the stream power law , 1999 .
[45] D. Merritts,et al. Interpreting Quaternary uplift rates at the Mendocino triple junction, northern California, from uplifted marine terraces. , 1989 .
[46] G. Tucker,et al. Dynamics of the stream‐power river incision model: Implications for height limits of mountain ranges, landscape response timescales, and research needs , 1999 .
[47] W. Dietrich,et al. Hillslope evolution by nonlinear creep and landsliding: An experimental study , 2001 .
[48] J. Roering,et al. How well can hillslope evolution models “explain” topography? Simulating soil transport and production with high-resolution topographic data , 2008 .
[49] Rafael L. Bras,et al. The Effect of Spatial Heterogeneities on Geomorphic Expression in a Model of Basin Evolution , 1995 .
[50] G. Parker,et al. Linear stability analysis of channel inception: downstream-driven theory , 2000, Journal of Fluid Mechanics.
[51] T. Hoey,et al. Surface process models and the links between tectonics and topography , 2006 .
[52] R. Bras,et al. Network‐scale dynamics of grain‐size sorting: implications for downstream fining, stream‐profile concavity, and drainage basin morphology , 2004 .
[53] Alan D. Howard,et al. Channel changes in badlands , 1983 .
[54] Paul Bishop,et al. Cenozoic river profile development in the Upper Lachlan catchment (SE Australia) as a test of quantitative fluvial incision models , 2003 .
[55] G. Tucker,et al. Channel response to tectonic forcing: field analysis of stream morphology and hydrology in the Mendocino triple junction region, northern California , 2003 .
[56] Per Bak,et al. Self-organized criticality in layered, lacustrine sediments formed by landsliding , 2002 .
[57] Gregory E. Tucker,et al. Bedrock channel adjustment to tectonic forcing: Implications for predicting river incision rates , 2007 .
[58] Kelin X. Whipple,et al. Topographic outcomes predicted by stream erosion models: Sensitivity analysis and intermodel comparison , 2002 .
[59] Dorothy J. Merritts,et al. Geomorphic response of coastal streams to low, intermediate, and high rates of uplift, Medocino triple junction region, northern California , 1989 .
[60] Robert S. Anderson,et al. Evolution of the Santa Cruz Mountains, California, through tectonic growth and geomorphic decay , 1994 .
[61] R. Anderson,et al. Modeling of knickpoint retreat on the Roan Plateau, western Colorado , 2007 .
[62] J. Roering. Soil creep and convex‐upward velocity profiles: theoretical and experimental investigation of disturbance‐driven sediment transport on hillslopes , 2004 .
[63] W. Davis. The Geographical Cycle , 1899 .
[64] G. Tucker,et al. New constraints on sediment-flux-dependent river incision: implications for extracting tectonic signals from river profiles , 2008 .
[65] G. Tucker. Drainage basin sensitivity to tectonic and climatic forcing: implications of a stochastic model for the role of entrainment and erosion thresholds , 2004 .
[66] S. Willett,et al. On steady states in mountain belts , 2002 .
[67] C. Paola,et al. Landscape instability in an experimental drainage basin , 2000 .
[68] Jeff Peakall,et al. Physical modelling in fluvial geomorphology: principles, applications and unresolved issues , 1996 .
[69] M. Brandon,et al. A Fluvial Record of Long-term Steady-state Uplift and Erosion Across the Cascadia Forearc High, Western Washington State , 2001 .
[70] Douglas W. Burbank,et al. Transient landscape evolution of basement‐cored uplifts: Example of the Kyrgyz Range, Tian Shan , 2007 .
[71] A. Howard. A detachment-limited model of drainage basin evolution , 1994 .
[72] K. Hodges,et al. The use of detrital mineral cooling ages to evaluate steady state assumptions in active orogens: An example from the central Nepalese Himalaya , 2005 .
[73] T. Hoey,et al. Quantification of the transient response to base-level fall in a small mountain catchment: Sierra Nevada, southern Spain , 2007 .
[74] G. Tucker,et al. Decoding temporal and spatial patterns of fault uplift using transient river long profiles , 2008 .
[75] M. Marden,et al. Tectonic and paleoclimatic significance of Quaternary river terraces of the Waipaoa river, east coast, North Island, New Zealand , 2000 .
[76] P. Bishop. Long‐term landscape evolution: linking tectonics and surface processes , 2007 .
[77] E. Kirby,et al. Characteristics of steady state fluvial topography above fault‐bend folds , 2007 .
[78] S. Schumm. EVOLUTION OF DRAINAGE SYSTEMS AND SLOPES IN BADLANDS AT PERTH AMBOY, NEW JERSEY , 1956 .
[79] G. Tucker,et al. Implications of sediment‐flux‐dependent river incision models for landscape evolution , 2002 .
[80] Philippe Fullsack,et al. Erosional control of active compressional orogens , 1992 .
[81] P. Beek,et al. Influence of incision rate, rock strength, and bedload supply on bedrock river gradients and valley-flat widths: Field-based evidence and calibrations from western Alpine rivers (southeast France) , 2006 .
[82] G. Tucker,et al. Importance of a stochastic distribution of floods and erosion thresholds in the bedrock river incision problem , 2003 .
[83] R. Anderson,et al. Hillslope Evolution by Bedrock Landslides , 1997, Science.
[84] Interactions between onshore bedrock-channel incision and nearshore wave-base erosion forced by eustasy and tectonics , 2002 .
[85] Stanley A. Schumm,et al. Experimental fluvial geomorphology , 1987 .
[86] Jérôme Lavé,et al. Fluvial incision and tectonic uplift across the Himalayas of central Nepal , 2001 .
[87] K. Whipple. BEDROCK RIVERS AND THE GEOMORPHOLOGY OF ACTIVE OROGENS , 2004 .
[88] G. Willgoose. Mathematical Modeling of Whole Landscape Evolution , 2005 .