http://www.nercdtp.leeds.ac.uk/projects/index.php?id806. Desert aeolian sedimentary systems are sensitive to changes in a wide range of environmental variables, including climate, sea level, sediment supply and tectonic factors.
The ice sheet margin around the Antarctic Peninsula receded rapidly from its Last Glacial Maximum (LGM) position on the continental shelf edge ~ 18 ka (Davies et al., 2012) to a position towards the head of fjords, and in some cases onto land.
Dr C Stevenson, Dr I Kane, Dr R Jerrett, Dr M Poyatos More
23 January 2019
Deep-water turbidite systems have transition zones where flows change their behaviour from bypassing to depositional, often associated with a break in slope and a distinct change in architecture from channels into lobes (i.e.