|
|
Geological conditions, reservoir evolution and favorable exploration directions of marine ultra-deep oil and gas in China
|
LI Jianzhong,TAO Xiaowan,BAI Bin,HUANG Shipeng,JIANG Qingchun,ZHAO Zhenyu,CHEN Yanyan,MA Debo,ZHANG Liping,LI Ningxi,SONG Wei
|
|
|
Table 1 Basic geological parameters of the marine ultra-deep oil and gas fields in China.
|
|
Basin | Oil and gas field | Buried depth/ m | Superimposed oil- and gas- bearing area/km2 | Proven crude oil reserves/ 104 t | Proven natural gas reserves/ 108 m3 | Reservoir types | Primary oil and gas layers | Reservoir lithologies | Effective thickness of reservoir/m | Poro- sity/% | Storage space | Structural location | Tarim | Halahatang | 5900- 7600 | 1 323 | 24 675 | 393 | Lithologic-stratigraphic | O2yj O1-2y | Sparite calcarenite, oolitic limestone | 6-25 | 1.8- 21.3/7.5 | Cave, vug, fracture | Periphery of Manxi intra- cratonic rift | Central Tarim No.1 | 4500- 6800 | 288 | 21 983 | 3 680 | O3l O1-2y | Sparite calcarenite, reef shoal limestone | 5-65 | 1.8- 16.0/4.6 | Tahe | 5300- 7000 | 2410 | 136 389 | 384 | O1-2y O2yj | Sparite calcarenite, oolitic limestone | 8-60 | 2.7- 75.0 | Shunbei | 7300- 8500 | 47 | 9903 | 216 | O1-2y O2yj | Sparite calcarenite | 3-30 | 2.6- 36.0 | Sichuan | Anyue | 4500- 5400 | 2691 | 3185 | 11 709 | Structural-lithologic | ?C1l Z2d | Algae dolomite, granular dolomite | 5-60 30-280 | 2.0- 18.5/4.8 2.0- 7.8/3.4 | Cave, vug, fracture | Periphery of Deyang-Anyue intracratonic rift | Longgang | 3680- 7286 | 156 | | 742 | P3ch T1f | Sparry oolitic dolomite | 6-35 | 3.7- 8.5/6.5 | Pore | Periphery of Kaijiang- Liangping Trough | Puguang | 4776- 7100 | 124 | | 4 121 | P3ch T1f | 101-411 | 2.0- 28.9/8.1 | Pore | Yuanba | 6250- 7367 | 549 | | 2 712 | P3ch T1f | 40-100 | 2.0- 23.6/5.2 | Pore |
|
|
|