Sedimentological parameters of the Holocene deposits in the Morsott area. The sedimentological parameters determined to the fine fraction, less than 2 mm, show variable mode, average, index asymmetry, and flattening values indicating a medium to high energy carrier current regime at the base of the series (unit K and L) and from medium to low during the Holocene.
|Designations||Breccias and pebbles set||Silty sands set||Sandy clayey silts set||Sandy silts set|
|Units||D, L||K, E||C, F, H, J||A, B, G, I|
|Mode in μm||500||350||380||400||Characteristics|
|Mean in μm||380||200||115||250||What reveals that the current transport has an average with weak energy|
|Sorting So||−0.1||−0.9||−0.5||−0.35||Grains very well classified|
|Skewnes Sk||−0.3||−0.42||−0.50||−0.45||The classification is better beside the fine particles|
|Kurtosis Ku||0.3||0.1||0.1||0.2||The curves are very platykurtic with heterogeneous composition|
|Classification according to Folk (1954)||Silty facies||Silty facies||Silty facies||Silty facies|
Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.
Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.
Initial download of the metrics may take a while.