“…But it is generally accepted that E 2 w and E 3 e are the most important source rocks in the PRMB (Zhu et al, 1999;Kang and Feng, 2011). In the Wenchang A depression, E 3 e is confirmed to be the primary source rock (Huang et al, 2003;Fu et al, 2011;Cheng et al, 2013a). The E 3 e, which is dominated by mixed type II 2 and III kerogens, has total organic carbon (TOC) contents between 0.27% and 8.4% (Fig.4A) and hydrocarbon generation potential (S 2 ) between 0.02 and 16.4 mg/g with medium hydrogen indices (usually lower than 400 mg/g, Fig.5A).…”