Figure 3
From: Diagenetic evolution of the Oligocene Huagang Formation in Xihu sag, the East China Sea Shelf Basin
Vertical variation of T, Th, Ro%, I/S-S%, Tmax in Xihu sag and diagenetic stage division. (A) Formation temperature; (B) homogenization temperature of inclusions; (C) vitrinite reflectance; (D) smectite content in the I/S mixed layer; (E) pyrolysis peak temperature.
