1. The organic matter content in CL is relatively low, with only a tiny amount of residual free oil distributed on the surface of intergranular pores of clay minerals (Fig. 10E). In AL, the clay filling pores is minimal, but a significant amount of solid bitumen is present among the particles, along with a substantial distribution of residual free oil along the laminae (Fig. 10F). Numerous intergranular pores filled with adsorbed oil and residual free oil are present in CDL;A;detrital organic matter, and solid bitumen are abundant in FL and ML (Fig. 10A-C), mixed with clay minerals, resulting in detrital quartz and feldspar appearing as if they are floating,2015
2. A mathematical representation of Rock-Eval hydrogen index vs T max profiles;A Banerjee;Org. Geochem,1998
3. The determination of pore volume and area distributions in porous substances: I. computations from nitrogen isotherms;E P Barrett;J. Am. Chem. Soc,1951
4. Early generation characteristics of a sulfur-rich Monterey kerogen;D K Baskin;Am. Assoc. Pet. Geol. Bull,1992
5. Adsorption of gases in multimolecular layers;S Brunauer;J. Am. Chem. Soc,1938