9 Sequence Stratigraphy

ravinement The findings provide insight into the processes of transgressive wave ravinement in a mixed carbonate and siliciclastic setting ona vastepicontinental shelf in an icehouse climate 2 Geological background The study area covers 4100 km2 from the limestone-rich Cherokee Platform in SE Kansas to the siliciclastic-

Reconstruction of Relative Tectonic Movements Using

ravinement surfaces are created by tidal erosion and called either “tidal ravinements” [8] or “bay ravinements” [1] The flattened ravinement surface is a useful reference plane for interpreting tectonic movements The ravinement surfaces can be assumed to be pretty much the same feature

Submerged shoreline preservation and ravinement during rapid

ravinement surface is attributed to fast sea-level rise (possibly associated with meltwater pulse 1B), while the gentle ravinement surface is associated with a subsequent slowing of the rate of sea-level rise (to 0 15 mm yr–1) Preservation of the main barrier and backbarrier

Giant Incised Valley Fill and Shoreface Ravinement Traps

Giant Incised Valley Fill and Shoreface Ravinement Traps, Urna, Ust-Teguss and Tyamskaya Field Areas, Southern West Siberian Basin, Russia* John Dolson1, S George Pemberton2, Sergey Hafizov3, Vera Bratkova4, Ekaterina Volfovich5, and Irina Averyanova5 Search and Discovery Article #10634 (2014)** Posted August 29, 2014

Transgressive Ravinement versus Depth of Closure: A

Transgressive ravinement versus depth of closure: a geological perspective from the upper Texas coast Journal of Coastal Research, 00(0), 000–000 West Palm Beach (Florida), ISSN 0749-0208

Analyse du ravinement de bassins versants à retenues

Le ravinement varie fortement selon les intensités des précipitations et le type d'oc cupation des sols des impluviums Au cours des quatre années de l'étude, le ravinement a fourni entre 15 et 65 m 3/ha/an de terre aux retenues Mots clés : érosion des sols, ravinement, sédimentation, retenues collinaires, suffosion, argiles gonflantes

Variations in shoreface progradation and ravinement along the

Keywords Foreshore, littoral drift, longshore current, ravinement, shoreface, transgression INTRODUCTION The shoreface environment is a transition zone between the foreshore and the inner shelf