New Insight into the Kinetics of Deep Liquid Hydrocarbon Cracking and Its Significance

Table 1

Basic geochemical characteristics of source rock samples.

Well	Strata	Depth (m)	Basin	TOC (%)	max (°C)	(mg/g)	(mg/g)	HI (mg/g·TOC)	(%)
Chao 73–87	K	834.6	Songliao Basin	4.89	435	1.39	42.06	860	0.5
Da 11	K	1710	Songliao Basin	3.71	434	0.91	30.74	829	0.5
Da 11	K	1712	Songliao Basin	4.14	442	0.74	36.70	886	0.6
Da 11	K	1722	Songliao Basin	3.31	447	0.51	27.19	821	0.8
X28	J	1996	Sichuan Basin	3.03	447	2.96	12.07	398	0.9
PL 10	J	1995	Sichuan Basin	2.54	449	3.65	10.21	402	1.0
PL10	J	1997	Sichuan Basin	2.81	449	2.45	10.40	370	1.0