In: Stratigraphy & Timescales, 2018, vol. 3, p. 151–187
The sedimentary record of ancient shallow-marine carbonate platforms commonly displays a stacking of different facies, which reflects repetitive changes of depositional environments through time. These changes can be induced by external factors such as cyclical changes in climate and/or sea level, but also by internal factors such as lateral migration of sediment bodies and/or changes in the...
|
In: Mathematical Geosciences, 2011, vol. 43, no. 3, p. 305-328
|
In: Swiss Journal of Geosciences, 2010, vol. 103, no. 1, p. 101-119
|