Conventional | Oil | Favorable traps at structural highs | Separate | Secondary | High abundance; stratigraphic and lithologic reservoirs | Regional and immediate caprock | Liquid hydrocarbon | 40%-80% movable hydrocarbon | Oil with high abundance, good reservoir properties and high natural production | Vertical and horizontal wells, etc. | 90%- 100% movable oil | 90%- 100% movable oil | 4 878 ×108 | 200× 108 | Gawal Oilfield, Daqing Oilfield |
Gas | Favorable traps at structural highs | Separate | Secondary | High abundance; stratigraphic and lithologic reservoirs | Regional and immediate caprock | Gas hydrocarbon, generally CH4 | 90%- 100% free gas | Oil with high abundance, good reservoir properties and high natural production | Vertical and horizontal wells, etc. | 90%- 100% free gas | 90%- 100% free gas | 471 ×1012 | 20× 1012 | North-South Pars Gas Field, Kela 2 Gas Field |
Retained | Heavy oil +asphalt | Near surface | Separate | Secondary | Favorable trap in the drainage area | Caprock and self- sealing | Heavy oil | Unmo- vable oil | Heavy oil with poor movability and no natural pro- duction | Steamflooding, gravity, steam stimulation, cooling production | Almost unmovable oil | Almost unmovable oil | 2 146 ×108 | 42× 108 | Heavy oil in Venezuela, asphalt sandstone in the Western Canada Basin |
Hydrate | Stable T and P zone | Separate | Secondary | Reservoir enrichment in coarse facies | T and P conditions | Domi- nant CH4 | Almost no free gas | Unconsolidated seabed pay zone, unstable and without natural production | Pressure drop, thermal production | Hardly free gas | Hardly free gas | 3 000 ×1012 | (50- 70)× 1012 | Hydrate in the northern part of the South China Sea |
Tight | Oil | Basin center or slope | Direct contact or neighbor | Primary or short secondary migration | High abundance in the tectonic or fractured zone | Good top and bottom | Matured oil | 20%-50% movable hydro- carbon | Tight reservoirs | Energizing, fracturing in horizontal wells | 90%- 100% movable oil | 90%- 100% movable oil | (400- 600) ×108 | (20- 25)× 108 | Triassic in Ordos Basin, Cretaceous tight sandstone oil in Songliao Basin, |
Gas | Basin center or slope | Direct contact or neighbor | Primary or short secondary migration | High abundance in the tectonic or fractured zone | Good top and bottom | Different gas saturation, almost 60% below | 90%- 100% free gas | Tight reservoirs with low natural production | Fracturing in horizontal wells | 90%- 100% free gas | 90%- 100% free gas | 210× 1012 | (9- 13)× 1012 | Carboniferous-Permian in Ordos Basin, Triassic tight sandstone gas in Sichuan Basin |
Source rock | Shale oil | Developed shale in deep sags or slopes | Same | No or short inside-source primary migration | Nano-pore and throat system, enrichment in the fracture development zone | Good top and bottom | Less mature oil and immature oil sand | 0%-30% movable hydrocarbon | Low or no production, low natural production | In-situ thermal transformation | 0%-100% movable oil | 0-5% movable oil | 15 000 ×108 | (200- 300)× 108 | Triassic shale oil in Ordos Basin |
Matured oil | 20%-50% movable hydrocarbon | Low or no production, low natural production | Fracturing in horizontal wells | 90%- 100% movable oil | 90%- 100% movable oil | Bakken shale oil in Wyckenston Basin |
Shale gas | Near basin subsidence-sedimenta- tion center | Same | No or short inside-source primary migration | Disperse distribution in shale, enrichment in fracture zones | Good top and bottom | Dry gas absorbed to kerogen, pores and free in fractures | 40%-70% free gas | Low production and recovery | Fracturing in horizontal wells | 80%- 100% free gas | 30%-60% free gas | 456× 1012 | (10- 25)× 1012 | Masalus shale gas in Appalachian Basin, Lower Paleozoic shale gas in Sichuan Basin |
CBM | Basin or de- pression synclines | Same | No or short inside-source primary migration | Enrichment in fractures and joints | Good top and bottom | Absorbed and free gas | 5%-20% free gas | Low production, no natural production | Fracturing in horizontal wells | 5%-10% free gas | 0-5% free gas | 256× 1012 | 11× 1012 | Carboniferous-Permian CBM in Qinshui and Ordos Basins |