A recursion model to calculate the original widths of narrow terraces and their backwearing rates in a coastal area subjected to regular uplift during the late Holocene
暂无分享,去创建一个
[1] A. Trenhaile. Modelling the effect of Pliocene–Quaternary changes in sea level on stable and tectonically active land masses , 2014 .
[2] S. Uesawa,et al. Quantitative estimation of erosion rate based on temporal change of rock coasts composed of volcanic deposit , 2014 .
[3] R. Castedo,et al. Modeling cyclic recession of cohesive clay coasts: Effects of wave erosion and bluff stability , 2013 .
[4] H. Viles,et al. Reconceptualising the role of organisms in the erosion of rock coasts: A new model , 2012 .
[5] Christophe Morhange,et al. Active Coastal Thrusting and Folding, and Uplift Rate of the Sahel Anticline and Zemmouri Earthquake area (Tell Atlas, Algeria) , 2011 .
[6] A. Trenhaile. Cliffs and Rock Coasts , 2011 .
[7] Hidekazu Tsujimoto,et al. Dynamic conditions for shore platform initiation , 2010 .
[8] L. Naylor,et al. Rock coast geomorphology: Recent advances and future research directions , 2010 .
[9] W. Stephenson. Discussion of de Lange, W. P. and Moon V. G. 2005. Estimating long-term cliff recession rates from shore platform widths. Engineering Geology 80, 292–301 , 2008 .
[10] A. Trenhaile. The development of subhorizontal shore platforms by waves and weathering in microtidal environments , 2008 .
[11] V. Moon,et al. Estimating long-term cliff recession rates from shore platform widths , 2005 .
[12] J. Hall,et al. A predictive Mesoscale model of the erosion and profile development of soft rock shores , 2005 .
[13] A. Trenhaile. Modelling the Quaternary evolution of shore platforms and erosional continental shelves , 2001 .
[14] A. Trenhaile. Modeling the effect of late Quaternary interglacial sea levels on wave-cut shore platforms , 2001 .
[15] W. Stephenson. Shore platforms: a neglected coastal feature? , 2000 .
[16] A. Trenhaile. Modeling the development of wave-cut shore platforms , 2000 .
[17] R. M. Kirk,et al. Development of shore platforms on Kaikoura Peninsula, South Island, New Zealand: II: The role of subaerial weathering , 2000 .
[18] K. Lambeck,et al. Refining the eustatic sea-level curve since the Last Glacial Maximum using far- and intermediate-field sites , 1998 .
[19] W. Stephenson,et al. MEASURING EROSION RATES USING THE MICRO-EROSION METER : 20 YEARS OF DATA FROM SHORE PLATFORMS, KAIKOURA PENINSULA, SOUTH ISLAND, NEW ZEALAND , 1996 .
[20] Y. Ota,et al. Age and Deformation of Marine Terraces on the Ashizuri Peninsula and its Vicinity, Southwestern Japan , 1994 .
[21] T. Sunamura,et al. Geomorphology of rocky coasts , 1992 .
[22] H. Maemoku,et al. Holocene Crustal Movement in the Southern Part of Kii Peninsula, Outer Zone of Southwest Japan , 1990 .
[23] M. Ishida. Seismicity in the South Fossa Magna and the northern margin of the Philippine Sea plate , 1990 .
[24] A. Trenhaile. The Geomorphology of Rock Coasts , 1987 .
[25] H. Kayanne,et al. Comparative Study between Present and Emergent Erosional Landforms on the Southeast Coast of Boso Peninsula, Central Japan , 1986 .
[26] A. S. Trenhaile,et al. Shore platforms: a neglected coastal feature , 1980 .
[27] T. Sunamura. A mathematical model of submarine platform development , 1978 .