Interaction between Crustal-Scale Darcy and Hydrofracture Fluid Transport: A Numerical Study

Table 3

Data and power-law fits of data shown in Figure 7.

	Volume of fractures reaching the surface (%)	Volume of fractures not reaching the surface (%)	No. of events reaching the surface	No. of events reaching the surface (%)	No. of events not reaching the surface	No. of events not reaching the surface (%)	Power-law fit for fractures not reaching the surface
	14.81	85.19	10	0.52	1,906	99.48
	2.78	97.22	34	0.19	18,197	99.81
	1.87	98.13	401	0.16	253,050	99.84
	1.87	98.13	393	0.15	251,940	99.84
	1.88	98.12	459	0.17	265,630	99.83
	2.93	97.06	447	0.25	179,091	99.75
	85.14	14.86	159	18.73	690	81.27
	97.99	2.00	15	75	5	25