Oil & Gas Geology ›› 2023, Vol. 44 ›› Issue (6): 1378-1392.doi: 10.11743/ogg20230604
• Petroleum Geology • Previous Articles Next Articles
Guangfu WANG1,2(), Fengxia LI1,2, Haibo WANG1,2, Tong ZHOU1,2, Yaxiong ZHANG1,2, Ruyue WANG1,2, Ning LI1,2, Yuxin CHEN1,2, Xiaofei XIONG1,2
Received:
2023-08-01
Revised:
2023-10-09
Online:
2023-12-01
Published:
2023-12-20
CLC Number:
Guangfu WANG, Fengxia LI, Haibo WANG, Tong ZHOU, Yaxiong ZHANG, Ruyue WANG, Ning LI, Yuxin CHEN, Xiaofei XIONG. Difficulties and countermeasures for fracturing of various shale gas reservoirs in the Sichuan Basin[J]. Oil & Gas Geology, 2023, 44(6): 1378-1392.
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Table 1
Statistics of geological and engineering parameters of shale gas reservoirs in different blocks[12-22]"
页岩气 类型 | 区块 | 构造位置 | 层系 | 岩石类型 | 沉积环境 | 埋深/m | 优质页岩 厚度/m | TOC/% | Ro/% | 含气量/(m3/t) | 孔隙度/ % | 石英 含量/% | 黏土矿物 含量/% | 泊松比 | 杨氏模量/ GPa | 水平应 力差/MPa | 压力 系数 | 天然裂缝 发育程度 |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
海相盆内中-浅层 超压页岩气 | 焦石坝 | 川东高陡褶皱带万县复向斜南部 | 志留系 龙马溪组 | 硅质页岩 | 深水陆棚 | 2 250 ~ 3 500 | 80 ~ 114 | 2.53 ~ 4.13 | 2.4 ~2.8 | 5.5 ~ 7.0 | 4.3 ~ 7.8 | 46.0 ~65.0 | 17.0 ~35.0 | 0.19 ~0.25 | 34.0 ~ 46.0 | 3.0 ~ 7.5 | 1.55 ~ 1.60 | 欠发育 |
长宁 | 川南褶皱带与娄山断褶带交界处 | 硅质页岩 | 半深水- 深水陆棚 | 2 300 ~ 3 200 | 29 ~ 38 | 3.00 ~ 5.00 | 2.1 ~2.9 | 2.9 ~ 7.4 | 4.0 ~ 7.0 | 46.4 ~63.0 | 23.9 ~32.1 | 0.16 ~0.27 | 25.0 ~ 36.0 | 10.0 ~ 16.0 | 1.20 ~ 2.00 | 欠发育- 发育 | ||
威远 | 川西南古中斜坡低褶带 | 含灰硅质 页岩 | 半深水- 深水陆棚 | 2 000 ~ 3 500 | 34 ~ 49 | 2.50 ~ 3.40 | 2.2 ~2.6 | 3.0 ~ 9.2 | 3.8 ~ 6.5 | 40.0 ~78.0 | 36.9 ~43.7 | 0.16 ~0.22 | 29.3 ~ 37.3 | 6.0 ~ 8.0 | 1.00 ~ 1.96 | 较发育 | ||
海相盆缘 深层常压 页岩气 | 白马 | 白马向斜 | 硅质页岩 | 深水陆棚 | 3 800 ~ 4 600 | 28 ~ 44 | 3.17 ~ 5.20 | 2.4 ~2.9 | 2.7 ~ 5.6 | 3.4 ~ 4.1 | 57.4 ~74.6 | 21.0 ~24.0 | 0.19 ~0.22 | 28.5 ~ 47.4 | 17.0 ~ 21.0 | 1.10 ~ 1.30 | 欠发育 | |
武隆 | 利川- 武隆复向斜 | 硅质页岩 | 深水陆棚 | 3 500 ~ 5 000 | 32 ~ 40 | 3.91 ~ 4.20 | 2.5 ~2.7 | 5.4 ~ 5.6 | 4.7 ~ 4.8 | 56.0 ~70.0 | 25.3 ~28.5 | 0.22 ~0.25 | 34.0 ~ 41.3 | 13.0 ~ 17.7 | 1.05 ~ 1.10 | 较发育 | ||
林滩场 | 齐岳山断裂以西,桑木场构造带上的次级背斜 | 硅质页岩、 粉砂质泥岩 | 深水陆棚 | 3 800 ~ 5 000 | 11 ~ 21 | 0.65 ~ 5.78 | 2.2 ~2.4 | 1.8 ~ 8.4 | 1.8 ~ 7.3 | 37.0 ~66.0 | 16.5 ~24.6 | 0.18 ~0.38 | 27.0 ~ 47.3 | 14.6 ~ 25.4 | 1.08 ~ 1.20 | 发育 | ||
海相盆内 深层超压 页岩气 | 江东 | 万县复向斜 东南部 | 硅质页岩 | 深水陆棚 | 3 577 ~ 4 350 | 37 ~ 44 | 2.30 ~ 3.15 | 2.4 ~2.8 | 3.5 ~ 4.5 | 3.6 ~ 5.2 | 56.0 ~74.4 | 22.4 ~54.7 | 0.20 ~0.22 | 29.1 ~ 36.0 | 7.0 ~ 8.5 | 1.45 ~ 1.70 | 发育 | |
威荣 | 川西南古中斜坡低褶带 | 含灰硅质 页岩 | 深水陆棚 | 3 500 ~ 4 500 | 27 ~ 39 | 2.50 ~ 3.20 | 2.4 ~2.6 | 2.6 ~ 8.7 | 4.7 ~ 7.4 | 41.5 ~58.3 | 24.5 ~46.0 | 0.22 ~0.25 | 21.6 ~ 27.3 | 11.0 ~ 16.0 | 1.80 ~ 2.00 | 较发育 | ||
永川 | 新店子背斜 | 硅质页岩 | 深水陆棚 | 3 800 ~ 4 200 | 27 ~ 39 | 1.11 ~ 7.83 | 2.2 ~2.5 | 1.5 ~ 8.3 | 2.2 ~ 2.5 | 46.0 ~52.8 | 23.9 ~32.1 | 0.19 ~0.23 | 20.0 ~ 31.8 | 7.4 ~ 25.4 | 1.77 ~ 2.10 | 欠发育- 发育 | ||
大足- 铜梁 | 西山背斜、蒲吕场向斜和西温泉背斜 | 硅质页岩、 灰质页岩 | 深水陆棚 | 4 086 ~ 5 800 | 29 ~ 66 | 1.30 ~ 5.60 | 2.4 ~3.1 | 3.6 ~ 5.7 | 3.4 ~ 5.9 | 51.6 ~68.3 | 10.6 ~58.8 | 0.19 ~0.26 | 27.2 ~ 45.3 | 13.0 ~ 18.0 | 1.95 ~ 2.04 | 较发育, 层理缝 发育 | ||
泸州 | 川南低褶构造带 | 硅质页岩 | 深水陆棚 | 3 540 ~ 3 625 | 32 ~ 65 | 2.80 ~ 3.30 | 2.4 ~3.5 | 3.6 ~ 5.7 | 4.4 ~ 5.7 | 55.0 ~72.1 | 25.5 ~47.2 | 0.13 ~0.24 | 26.0 ~ 45.0 | >20.0 | 1.86 ~ 2.05 | 层理缝 发育 | ||
丁山 | 丁山断鼻 | 炭质页岩、 硅质页岩 | 深水陆棚 | 3 727 ~ 4 367 | 39 ~ 35 | 1.90 ~ 3.80 | 2.0 ~2.2 | 2.0 ~ 3.7 | 4.5 ~ 6.0 | 42.5 ~57.1 | 7.2 ~ 43.5 | 0.20 ~0.22 | 27.6 ~ 32.3 | 22.0 ~ 27.0 | 1.78 ~ 1.90 | 发育 | ||
东溪 | 川东南东溪高陡构造 | 硅质页岩 | 深水陆棚 | 4 058 ~ 4 335 | 26 ~ 30 | 2.43 ~ 3.62 | 2.1 ~2.5 | 5.1 ~ 7.8 | 3.2 ~ 6.3 | 46.0 ~62.0 | 18.5 ~45.0 | 0.19 ~0.28 | 32.0 ~ 43.0 | 15.0 ~ 24.0 | 1.60 ~ 1.80 | 发育 | ||
海相新类型页岩气 | 井研- 犍为 | 绵阳-长宁拉张 槽西侧宽缓 斜坡带 | 寒武系 筇竹寺组 | 页岩、粉砂质泥岩、泥质粉砂岩 | 深水-浅水 陆棚 | 3 235 ~ 3 591 | 104 | 0.11 ~ 2.10 | 2.2 ~5.6 | 0.1 ~ 3.3 | 0.8 ~ 4.5 | 66.8 ~81.7 | 20.1 ~28.8 | 0.18 ~0.23 | 34.3 ~ 46.4 | 4.0 ~ 9.1 | 1.30 ~ 1.50 | 欠发育 |
海-陆过渡相盆内超压页岩气 | 普光 大隆 | 川东北滑脱褶 皱带 | 二叠系 大隆组 | 泥岩、含灰 泥岩 | 浅水-深水 陆棚 | 3 500 ~ 4 600 | 18 ~ 35 | 3.24 ~ 5.82 | 2.0 ~3.1 | 4.5 | 0.6 ~ 4.9 | 38.0 ~52.3 | 4.3 ~ 9.4 | 0.23 ~0.27 | 36.0 ~ 57.6 | 9.7 ~ 10.4 | 1.65 ~ 1.68 | 较发育 |
红星 | 川东高陡褶皱带石柱复向斜建南构造 | 二叠系 吴家坪组 | 页岩、白云质灰岩 | 深水-斜坡浅水陆棚 | 3 300 ~ 3 500 | 33 | 0.20 ~ 9.04 | 2.0 ~2.1 | 0.3 ~ 9.4 | 1.7 ~ 9.7 | 22.5 ~57.4 | 5.0 ~ 38.0 | 0.22 ~0.25 | 40.1 ~ 58.8 | 8.2 ~ 14.8 | 1.15 ~ 1.30 | 层理缝 发育 | |
陆相盆缘超压页岩气 | 复兴 | 川东高陡褶皱带万县复向斜 | 侏罗系 自流井组 | 黏土质页岩 | 半深湖- 浅湖 | 2 000 ~ 3 000 | 25 ~ 30 | 1.88 ~ 2.04 | 1.5 ~1.9 | 0.8 ~ 1.6 | 3.7 ~ 4.1 | 20.4 ~60.6 | 43.6 ~59.0 | 0.23 ~0.29 | 20.0 ~ 26.0 | 5.07 ~ 6.16 | 1.70 ~ 2.05 | 不发育 |
普光 千佛崖 | 普光东向斜低缓 单斜构造 | 侏罗系 千佛崖组 | 夹粉砂岩、 介壳层 | 湖泊 | 2 500 ~ 3 700 | 22 ~ 26 | 1.42 | 1.9 ~2.2 | 1.4 ~ 4.2 | 5.4 | 29.6 | 56.0 | 0.23 | 31.5 | 4.0 ~ 9.0 | 1.32 | 发育 | |
元坝 | 川东弧形褶皱带叠加区 | 侏罗系 自流井组 | 深灰色泥岩、深灰色粉砂质泥岩 | 半深湖- 浅湖 | 3 800 ~ 4 500 | 30 ~ 130 | 1.05 | 1.7 | 3.0 | 3.9 | 46.8 | 24.9 | 0.25 | 25.0 | 15.0 | 1.88 | 发育 |
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