“…Based on major parallel unconformities, the Palaeogene unit of the Fushan Depression is divided into three formations: the Changliu Formation (SQEch) of Early Eocene age, the Liushagang Formation (SQEls) of Middle to Late Eocene age, the Weizhou Formation (SQEwz) of Oligocene age (Fig.3) (Li et al, 2010;Liu et al, 2012;Liu et al, 2014). Using the sequence stratigraphic principles of Vail (1977), in combination with modern sedimentology techniques and sequence stratigraphic data (e.g.…”