Titlebook: Sand and Gravel Spits; Giovanni Randazzo,Derek W.T. Jackson,J. Andrew G. Book 2015 Springer International Publishing Switzerland 2015 Coa

Ballerina

The Development and Management of the Dingle Bay Spit-Barriers of Southwest Ireland,y an ebb-tidal delta and probably formed as a single barrier in the early- to mid-Holocene across Dingle Bay, before moving by . mechanisms to their present positions. Extensive back-barrier wetlands began to form behind this structure in the mid-Holocene. This earlier barrier was breached c. 3,000 

Suggestions

Sandy Spits and Their Mathematical Modeling, well as the effect of sand transport through an inlet that erodes the tip of the spit. Two field cases constituting more complex sand transport conditions at inlets, where different morphological features interacted with the spit evolution, were also investigated, but numerical approaches were empl

GUMP

Long-, Mid- and Short-Term Evolution of Coastal Gravel Spits of Brittany, France,For the swash-aligned gravel spits, frequency and magnitude of overwash processes is controlling the rate of landward retreat by rollover. This morphodynamic behaviour is illustrated by topo-morphological surveys realised between 2002 and 2012 on Sillon de Talbert spit which has experienced a comple

Customary

Morphological Characterization and Evolution of Tahadart Littoral Spit, Atlantic Coast of Morocco,volution was revealed by examining changes between the earliest (1981) and the latest (2007) shoreline positions. Accretion clearly prevailed over erosion and was particularly so in the northern part of the littoral (95 m, 3.7 m/year), at the river mouth (90 m, 3.5 m/year) and at southern part (the

Lineage

Geomorphology and Internal Sedimentary Structure of a Landward Migrating Barrier Spit (Southern Syler involving an interplay of barrier retreat and washover associated with accumulation of sediment in a backbarrier environment as a result of storm surges. With the exception of the uppermost dune facies the spit add-on zone reveals a transgressive coarsening upward sequence starting with sandy mud

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核心

ave to be further tested in wider clinical studies. Also, the objective criterion of “tumour shrinkage” and the duration of “progression free survival” (PFS) represent the commonest endpoints for phase III clinical trials, aiming to assess the benefit of applying one or more therapeutic schemes in s

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Gustavo Gabriel Bujalesky,Gustavo Gonzalez Bonorinohave to be further tested in wider clinical studies. Also, the objective criterion of “tumor shrinkage” and the duration of “progression free survival” (PFS) represent the commonest endpoints for phase III clinical trials, aiming to assess the benefit of applying one or more therapeutic schemes in s