Review Article

Lower Cambrian Organic-Rich Shales in Southern China: A Review of Gas-Bearing Property, Pore Structure, and Their Controlling Factors

Table 3

Pore structure parameters of the Lower Paleozoic shales in southern China (see Figure 2 for well locations).

RegionsFormationWellBuried depth (m)Number of samplesSpecific surface area (m2/g)
Range/Average
Total pore volume (mL/g)
Range/Average
Porosity (%)
Range/Average
References

Sichuan BasinWufeng-Longmaxi Fm.N2032170-2393287.3-31.8/14.920.03-0.06/0.0501.46-8.22/4.72[96]
Wufeng-Longmaxi Fm.W2011490-155266.2-20.2/14.000.03-0.07/0.0473.79-6.75/5.96
Longmaxi Fm.JY12288-23571014.3-32.1/23.300.02-0.03/0.0243.66-5.65/4.68[126]
Longmaxi Fm.JY22552-2607618.9-25.9/23.840.02-0.024/0.0223.43-4.73/4.17
Qiongzhusi Fm.W2012705-281692.3-10.8/5.900.01-0.04/0.0281.62-2.17/1.85[96]
Qiongzhusi Fm.N2061830-188794.5-9.6/7.640.03-0.04/0.0380.47-2.57/1.52
Qiongzhusi Fm.B12819-297793.9-7.0/5.140.02-0.03/0.0281.50-1.87/1.64
Qiongzhusi Fm.YS1063260-338072.0-3.4/2.640.01-0.03/0.0200.88-2.13/1.48

Western HubeiShuijingtuo Fm.YY11809-187167.2-18.2/14.000.01-0.04/0.0250.96-3.33/2.08[44]

Northwestern HunanNiutitang Fm.CY1795-133470.8-7.4/3.000.001-0.01/0.0051.20-1.80/1.50[21]

Northern GuizhouNiutitang Fm.TM11430-1457410.6-15.2/12.800.008-0.01/0.010nd[127]
Niutitang Fm.CY11418-144048.3-13.3/11.430.004-0.02/0.008nd

Southern AnhuiHetang Fm.XY1nd154.3-7.50.006-0.0120.30-2.82/1.47[24]

Note: “nd” means not detected.