| ZEIT BAY buried hill oil and gas field in Gulf of Suez | Quartz diorite, granodiorite,
granite, alkali granite, andesite
porphyry | The storage space is mainly composed of fractures, the development of which is controlled by faulting, diagenesis and inclination and direction of dyke and brecciated zone | Oil reservoir: 295 m,
gas reservoir: 70 m |
| Bonger rift basins in Central Africa rift valley | Cataclastic migmatitic granite,
migmatitic granite, and syenite | The storage space is made up of fractures and dissolved
pores, weathered crust and fracture belt form bi-layer
structure of reservoir in the bedrock | Greater than 300 m |
| Jatibarang oil and gas field in Indonesia | Faulted volcanic rock, including
andesite, basalt, tuff, volcanic
breccia and agglomerate | With fractures, intergranular pores and intercrystalline
pore as main storage space, the reservoirs feature
strong heterogeneity and abundant fractures | Gas reservoir: 1200 m |
| Anyue gas field in Sichun Basin | Granular dolomite and
crystalline dolomite | Dissolved pores, caves, fractures and structural
fractures constitute storage space | Up to 450 m |
Kelameili gas field
in Junggar Basin | Basic-intermediate basalt,
andesite, acid rhyolite, volcani-
clastic rock and orthophyre | The storage space includes secondary dissolved pores
and structural fractures, volcanic breccia and basalt
form high quality reservoirs | Approximately 250 m |
| Xushen gas field in Songliao Basin | Volcanic lava and
volcaniclastic rock | The storage space is made up of gas pores, dissolved
pores and high-angle and reticular fractures | 70-400 m |
| BZ19-6 condensate gas field in the Bohai Bay Basin | Gneiss, metamorphic granite,
migmatite, cataclasite and
morbruk rock | The storage space is composed of structural
fractures, intragranular fractures,
dissolved pores and dissolved fractures | Greater than 1500 m |