Good points. Unfortunately, it has to be kind of basic. Deltaic deposits could consume a career in geology. The thing that makes it easier is the presence of those transgressive sands. I am familiar with the 20 Mile Sandstone in the Willaims Fork Formation of Colorado. A great marker bed and easy geology. Some nice fossils too.
They tend to preserve nice seams below them. There are some regressive sands above, usually disncontinuous and much thinner.
So, for the layman, think of the delta deposits as a kind of swamp, partly marine partly terrestrial. The coal seams would represent a swampy area of high organic content ... and a river runs through it ... The beach is always there on a delta because waves wash the silt away and that sand moves along the shore with currents to form beaches far away. As the sea level rises, the beach moves inland until the high stand is reached and the sea recedes again. This happened numerous times in North America during the late Paleozoic and again in the late Cretaceous. Not sure what/ when happened in South Africa.