Oil & Gas Geology ›› 2022, Vol. 43 ›› Issue (1): 26-33.doi: 10.11743/ogg20220102
• Petroleum Geology • Previous Articles Next Articles
Received:
2020-11-03
Revised:
2021-12-20
Online:
2022-02-01
Published:
2022-01-28
CLC Number:
Qingfan Zhou. Discussion on key issues of shale oil/gas resource assessment[J]. Oil & Gas Geology, 2022, 43(1): 26-33.
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Table 2
Statistics of oil recovery factors for shale/tight oil plays selected in the U.S. [30]"
盆地 | 地层组/区带 | 地质年代 | 页岩油/致密油采收率/% |
---|---|---|---|
威利斯顿 | Bakken ND Core | 密西西比纪—泥盆纪 | 8.40 |
Bakken ND Ext. | 密西西比纪—泥盆纪 | 7.70 | |
Bakken MT | 密西西比纪—泥盆纪 | 3.90 | |
Three Forks ND | 泥盆纪 | 8.20 | |
Three Forks MT | 泥盆纪 | 3.60 | |
马弗里克 | Eagle Ford Play #3A | 晚白垩世 | 8.10 |
Eagle Ford Play #3B | 晚白垩世 | 9.00 | |
Eagle Ford Play #4A | 晚白垩世 | 4.20 | |
Eagle Ford Play #4B | 晚白垩世 | 5.80 | |
沃斯堡 | Barnett Combo?Core | 晚白垩世 | 1.50 |
Barnett Combo?Ext. | 密西西比纪 | 1.80 | |
二叠 | Del.Avalon/BS (NM) | 二叠纪 | 1.90 |
Del.Avalon/BS (TX) | 二叠纪 | 2.10 | |
Del.Wolfcamp (TX Core) | 二叠纪—宾西法尼亚纪 | 3.40 | |
Del.Wolfcamp (TX Ext.) | 二叠纪—宾西法尼亚纪 | 1.30 | |
Del.Wolfcamp (NM Ext.) | 二叠纪—宾西法尼亚纪 | 2.40 | |
Midl.Wolfcamp Core | 二叠纪—宾西法尼亚纪 | 1.90 | |
Midl.Wolfcamp Ext. | 二叠纪—宾西法尼亚纪 | 1.60 | |
Midl.Cline Shale | 宾西法尼亚纪 | 2.80 | |
阿纳达科 | CanaWoodford?Oil | 晚泥盆世 | 8.40 |
Miss.Lime?Central OK Core | 密西西比纪 | 3.10 | |
Miss.Lime?Eastern OK Ext. | 密西西比纪 | 0.60 | |
Miss.Lime?KS Ext. | 密西西比纪 | 1.30 | |
阿巴拉契亚 | Utica Shale?Oil | 奥陶纪 | 2.10 |
D-J | Niobrara Core | 晚白垩世 | 2.10 |
Niobrara East Ext. | 晚白垩世 | 1.20 | |
Niobrara North Ext.#1 | 晚白垩世 | 4.60 | |
Niobrara North Ext.#2 | 晚白垩世 | 0.90 | |
Niobrara North Ext.#2 | 晚白垩世 | 0.90 |
Table 3
Comparison of two main methods for shale oil/gas resources assessment[34-35,40,51]"
评价方法 | 优点 | 缺点 |
---|---|---|
基于页岩油气层含油气量的地质资源量评价方法 | 适用范围广,也适用勘探开发不成熟的新区;地质资料和科技进步因素易于反映到评价中 | 不能直接计算可采资源量;因需通过采收率转换,增加了可采资源评价结果的不确定性 |
基于单井页岩油气EUR的技术可采资源量评价方法 | 直接计算可采资源量,避免因估算可采系数不确定性的影响;评价结果更符合生产实际 | 通常需要大量生产数据;没有考虑未来技术进步因素的影响;不能直接用于勘探开发程度低的新区 |
Table 4
Shale gas resources assessment results in the Sichuan Basin and on its periphery, China[6,34-35,44]"
时间 | 机构 | 方法 | 评价层系 | 技术可采资源量/ (1012ft3) |
---|---|---|---|---|
2011 | EIA/ARI | 体积法 | 下寒武统筇竹寺组、 | 692.0 |
下志留统龙马溪组 | ||||
2013 | EIA/ARI | 体积法 | 下寒武统筇竹寺组、 | 625.9 |
下志留统龙马溪组、 | ||||
二叠系 | ||||
2015 | USGS | FORSPAN法 | 下寒武统筇竹寺组、 | 23.9 |
下志留统龙马溪组、 | ||||
二叠系龙潭组 | ||||
2012 | 国土资源部 | 体积法 | 寒武系、志留系、二叠系、三叠系、侏罗系 | 227.4 |
2015 | 国土资源部 | 体积法 | 寒武系、志留系、二叠系、三叠系、侏罗系 | 398.3 |
Table 5
Assessment results of shale gas resources in the Arkoma Basin and Alaska North Slope in the U.S.[51]"
页岩区带 | FORSPAN | 体积法 | ||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|
技术可采资源量 | 地质资源量 | 技术可采资源量 | ||||||||||
F95 | F50 | F5 | 均值 | P95 | P50 | P5 | 均值 | P95 | P50 | P5 | 均值 | |
Woodford | 6.06 | 10.16 | 17.04 | 10.68 | 347.0 | 148.0 | 49.5 | 171.3 | 34.70 | 14.80 | 4.95 | 17.13 |
Shublik | 0 | 36.60 | 72.20 | 38.40 | 1186.0 | 293.0 | 56.5 | 413.0 | 118.60 | 29.30 | 5.65 | 41.30 |
Brookian | 0 | 2.12 | 4.37 | 2.18 | 117.0 | 36.0 | 36.0 | 43.0 | 11.70 | 3.60 | 3.60 | 4.30 |
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