“Exploring petroleum inside source kitchen”: Connotation and prospects of source rock oil and gas
Zhi YANG,Caineng ZOU
Table 4 Comparison of main parameters of CBM in China and abroad.
Basin Geology Geochemistry
Basin type Sed. background Formation Depth/
m
Area/
km2
Net coal seams/m Gas genesis C1 isotope/
Ro/
%
Coal rank
Qinshui Cratonic Transitional Carboniferous-Permian 300-2 000 5 000 4-17 Thermal -31.95 1.5-3.0 Thin coal, lean coal, anthracite
Ordos Cratonic Transitional Carboniferous-Permian 600-2 000 10 000 5-18 Thermal -32.41 1.2-2.8 Coking coal, lean coal
Fenhe Foreland Swamp Paleogene 60-760 3 300 24-45 Biogenetic -62.33 0.3-0.4 Subbituminous coal
San Juan Foreland Transitional Cretaceous 150-1 200 1 900 9-21 Thermal and less biogenetic -41.12 0.3-1.3 High and low volatile bituminous coal
Basin Reservoir Fluid Resource Production
Pore Permeability/
10-3 μm2
Pressure coefficient CH4/% Gas/
(m3·t-1)
Recoverable resources/
108 m3
Abundance/
(108 m3?km-2)
Production/well/
(104 m3·d-1)
Yearly production/108 m3
Qinshui Nano-pores 0.01-5.75 0.7-0.9 98.87 4.0-32.0 6 064 1.2 0.2-0.3 30.9
Ordos Nano-pores 0.02-16.17 0.8-1.0 90.80 4.0-20.0 11 481 1.1 0.2-0.7 10.4
Fenhe Nano-pores 35.00-1 000.00 0.9-1.0 98.60 0.8-1.6 6 600 2.0 0.5-0.6 145.0
San Joan Nano-pores 5.00-60.00 1.0-1.2 97.00 10.0-12.7 3 800 2.0 1.0-3.0 150.0