Major Factors Controlling the Accumulation and High Productivity of Marine Shale Gas and Prospect Forecast in Southern China
-
摘要: 近年来我国在四川盆地率先实现了页岩气商业开发，奥陶系五峰组-志留系龙马溪组成为南方海相页岩气开发的主力层系.通过梳理页岩气沉积与分布特征、构造演化特征、构造样式及保存特征、页岩储层特征，提出了我国南方海相页岩气富集高产的主控因素：深水陆棚相富有机质优质页岩是物质基础；构造抬升时间和构造样式是页岩气富集保存的关键因素，总结了构造保存完整型、残留型、破坏型3大类页岩气构造样式；地层超压是页岩气高产的必要条件.最终展望了页岩气发展前景，预测了我国南方几个古隆起的边缘和滇黔桂地区是未来页岩气勘探开发的有利区.Abstract: Sichuan basin has been taking the lead in China for the shale gas business development in recent years. Ordovician Wufeng Formation-Silurian Longmaxi Formation has been the main layer of marine shale gas development in the south. Based on the analysis of shale gas deposition and distribution, tectonic evolution, tectonic patterns and preservation, shale reservoir characteristics, the main controlling factors on enrichment and high-production of marine shale gas are summarized. The rich organic shale formed in deep shelf sedimentary environment is taken of the main factor as the material basis. The time and style of tectonic uplift are the key factors of shale gas accumulation and preservation. Three types of shale gas tectonic styles are determined, including intact type, residual type and destructive type. Overpressure of formation is a necessary condition of high shale gas production. In this paper the prospect of shale gas in South China has been forecasted. Edges of paleo-highs and Yunnan-Guizhou-Guangxi region are predicted as the favorable areas for future exploration and development of shale gas.
-
Key words:
- shale gas /
- enrichment /
- high-production /
- main controlling factor /
- tectonic style /
- storage conditions /
- petroleum geology
-
图 1 我国南方下志留统龙马溪组页岩沉积相及厚度等值线
Fig. 1. Sedimentary facies and thickness of lower Silurian Longmaxi Formation shale in southern China
图 2 五峰-龙马溪组沉积微相及笔石发育特征
Fig. 2. Sedimentary microfacies and graptolite development characteristics of Wufeng Formation-Longmaxi Formation
图 3 五峰-龙马溪组页岩有机质孔发育
a.有机质孔，焦页1井，2 385.42 m；b.有机质孔，焦页2井，2 570.04 m
Fig. 3. Organic pores in well samples of Wufeng Formation-Longmaxi Formation
图 4 焦页1井五峰-龙马溪组综合评价
引自项目报告《涪陵页岩气勘探开发技术攻关与示范应用》，中国石化江汉油田分公司，2015
Fig. 4. The comprehensive evaluation of Wufeng Formation-Longmaxi Formation of well JY1
图 5 四川盆地及周缘构造纲要(a)及磷灰石裂变年龄演化(b)
Fig. 5. Tectonic outline (a) and age distribution based on apatite fission track (b) in the Sichuan basin and adjacent area
图 6 焦页1井和彭页1井生气及沉积埋藏史模拟
Fig. 6. The gas generating and depositional and burial history of well JY1 and well PY1
图 8 龙马溪组页岩地层压力系数与产量的关系
Fig. 8. The relation of pressure coefficient and shale gas production of Longmaxi Formation shale
图 9 我国南方古隆起边缘页岩气有利区划分
Fig. 9. Illustration of favorable shale gas zone selected in periphery of paleo-uplift in southern China
表 1 四川盆地及周缘典型页岩气井的压力系数与产量
Table 1. The pressure coefficient and production of shale gas well in the Sichuan basin and adjacent area
井号 压力系数 产量(104·m3·d-1) 焦页1HF 1.45 20.3 焦页27-1 1.45 34.3 焦页27-2 1.47 26.1 焦页27-3 1.54 33.5 焦页27-4 1.54 37.5 焦页29-1 1.63 35.6 焦页20-1 1.46 31.4 焦页20-2 1.49 34.8 焦页3-2 1.47 23.8 焦页3-3 0.97 14.5 焦页16-3 1.28 14.1 焦页29-3 1.51 31.8 焦页29-4 1.55 41.4 DY2HF 1.60 10.5 彭页1HF 0.96 2.3 彭页3HF 0.96 3.2 彭页4HF 0.94 1.7 南页1HF 1.50 0.2 威201-H1 0.92 1.3 威201 0.92 0.3 威202 1.40 2.8 威204 1.96 16.5 宁201-H1 2.03 15.0 长宁H2-1 1.79 8.0 长宁H2-2 1.58 21.0 长宁H2-3 1.62 8.3 长宁H2-4 1.60 13.4 长宁H3-1 1.93 7.7 长宁H3-2 1.92 7.7 长宁H3-3 1.96 5.6 阳201-H2 2.20 43.0 YSH1-1 1.15 3.6 YS108H1-1 2.00 20.7 保页1井 1.00 0.2 龙参2井 1.00 0.2 昭101 0.80 微含气 
下载: 导出CSV
-
[1] Chen, S.B., Zhu, Y.M., Wang, H.Y., et al., 2011.Characteristics and Significance of Mineral Compositions of Lower Silurian Longmaxi Formation Shale Gas Reservoir in the Southern Margin of Sichuan Basin.Acta Petrolei Sinica, 32(5):775-782 (in Chinese with English abstract). http://d.g.wanfangdata.com.cn/Periodical_syxb201105006.aspx [2] Curtis, J.B., 2002.Fractured Shale-Gas Systems.AAPG Bulletin, 86:1921-1938.doi: 10.1306/61eeddbe-173e-11d7-8645000102c1865d [3] Dong, D.Z., Cheng, K.M., Wang, Y.M., et al., 2010.Forming Conditions and Characteristics of Shale Gas in the Lower Paleozoic of the Upper Yangtze Region, China.Oil & Gas Geology, 31(3):288-299, 308 (in Chinese with English abstract). https://www.researchgate.net/publication/284617068_Forming_conditions_and_characteristics_of_shale_gas_in_the_Lower_Paleozoic_of_the_Upper_Yangtze_region_China [4] Guan, X.X., Yi, X.Y., Yang, H.H., 2014.Contrast of Shale Gas Reservoir Conditions in China and the United States.Journal of Southwest Petroleum University (Science & Technology Edition), 36(5):33-39 (in Chinese with English abstract). https://www.researchgate.net/publication/281750200_Contrast_of_shale_gas_reservoir_conditions_in_China_and_the_United_States [5] Guo, T.L., Zhang, H.R., 2014.Formation and Enrichment Mode of Jiaoshiba Shale Gas Field, Sichuan Basin.Petroleum Exploration and Development, 41(1):28-36 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SKYK201401003.htm [6] Guo, X.S., 2014.Rules of Two-Factor Enrichment for Marine Shale Gas in Southern China-Understanding from the Longmaxi Formation Shale Gas in Sichuan Basin and Its Surrounding Area.Acta Petrolei Sinica, 88(7):1209-1218 (in Chinese with English abstract). https://www.researchgate.net/publication/308340530_Formation_and_destruction_mechanism_as_well_as_major_controlling_factors_of_the_Silurian_shale_gas_overpressure_in_the_Sichuan_Basin_China [7] Guo, X.S., Guo, T.L., Wei, Z.H., et al., 2012.Thoughts on Shale Gas Exploration in Southern China.Engineering Sciences, 14(6):101-105, 112 (in Chinese with English abstract). [8] Hu, D.F, Zhang, H.R, Ni, K., et al., 2014.Main Controlling Factors for Gas Preservation Conditions of Marine Shale in Southeastern Margins of the Sichuan Basin.Natural Gas Industry, 34(6):17-23 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-TRQG201406003.htm [9] Jarvie, D.M., Hill, R.J., Ruble, T.E., et al., 2007.Unconventional Shale-Gas Systems:The Mississippian Barnett Shale of North-Central Texas as One Model for Thermogenic Shale-Gas Assessment.AAPG Bulletin, 91(4):475-499.doi: 10.1306/12190606068 [10] Jiang, C.P., Lei, Y.J., Gong, J., et al., 2011.Shale Gas Accumulation Conditions and Distribution and Prospect in China.Inner Mongolia Petrochemical Industry, 18:133-135 (in Chinesewith English abstract). [11] Li, X., Duan, S.K., Sun, Y., et al., 2011.Advances in the Exploration and Development of U.S. Shale Gas.Nature Gas Industry, 31(8):124-126 (in Chinese with English abstract). https://www.researchgate.net/publication/295960302_Advances_in_the_exploration_and_development_of_US_shale_gas [12] Li, X.J., Hu, S.Y., Cheng, K.M., 2007.Suggestions from the Development of Fractured Shale Gas in North America.Petroleum Exploration and Development, 34(4):392-400 (in Chinese with English abstract). https://www.researchgate.net/publication/279937654_Suggestions_from_the_development_of_fractured_shale_gas_in_North_America [13] Li, X.J., Lu, Z.G., Dong, D.Z., et al., 2009.Geologic Controls on Accumulation of Shale Gas in North America.Natural Gas Industry, 29(5):27-32 (in Chinese with English abstract). https://www.researchgate.net/publication/281392655_Geologic_controls_on_accumulation_of_shale_gas_in_North_America [14] Li, X.T., Shi, W.R., Guo, M.Y., et al., 2014.Characteristics of Marine Shale Gas Reservoirs in Jiaoshiba Area of Fuling Shale Gas Field.Journal of Oil and Gas Technology, 36(11):11-15 (in Chinese with English abstract). https://www.researchgate.net/publication/303145539_Characteristics_of_marine_shale_gas_reservoirs_in_Jiaoshiba_area_of_Fulin_shale_gas_field [15] Liang, D.G., Guo, T.L., Chen, J.P, et al., 2009.Some Progresses on Studies of Hydrocarbon Generation and Accumulation in Marine Sedimentary Regions, Southern China (Part 3):Controlling Factors on the Sedimentary Facies and Development of Palaeozoic Marine Source Rocks.Marine Origin Petroleum Geology, 14(2):1-19 (in Chinese with English abstract). [16] Liu, J., Xu, H.T., Yu, G., et al., 2014.Development Indices and Potential of Shale Gas, Sichuan Basin.Natural Gas Exploration & Development, 37(2):45-47, 52 (in Chinese with English abstract). [17] Nie, H.K., Tang, X., Bian, R.K., 2009.Controlling Factors for Shale Gas Accumulation and Prediction of Potential Development Area in Shale Gas Reservoir of South China.Acta Petrolei Sinica, 30(4):484-491 (in Chinese with English abstract). https://www.researchgate.net/publication/279571586_Controlling_Factors_for_Shale_Gas_Accumulation_and_Prediction_of_Potential_Development_Area_in_Shale_Gas_Reservoir_of_South_ChinaJ [18] Nie, H.K., Zhang, J.C., Bao, S.J., et al., 2012.Shale Gas Accumulation Conditions of the Upper Ordovician-Lower Silurian in Sichuan Basin and Its Periphery.Oil & Gas Geology, 33(3):335-345 (in Chinese with English abstract). [19] Tan, L.Y., Xu, Y., Li, D.H., et al., 2015.Geological Condition of Shale Gas Accumulation and Favorable Area Prediction for the Wufeng-Longmaxi Formations in Southeastern Chongqing.Acta Geologica Sinica, 89(7):1308-1317 (in Chinese with English abstract). [20] Wang, H.Y., Guo, W., Liang, F., et al., 2015.Biostratigraphy Characteristics and Scientific Meaning of the Wufeng and Longmaxi Formation Black Shales at Well Wei 202 of the Weiyuan Shale Gas Field, Sichuan Basin.Journal of Stratigraphy, 39(3):289-293 (in Chinese with English abstract). [21] Wang, S.J., Wang, L.S., Huang, J.L., et al., 2009.Accumulation Conditions of Shale Gas Reservoirs in Silurian of the Upper Yangtze Region.Natural Gas Industry, 29(5):45-50, 137 (in Chinese with English abstract). https://www.researchgate.net/publication/284098473_Accumulation_conditions_of_shale_gas_reservoirs_in_Silurian_of_the_Upper_Yangtze_region [22] Wang, S.J., Yang, T., Zhang, G.S., et al., 2012.Shale Gas Enrichment Factors and the Selection and Evaluation of the Core Area.Engineering Sciences, 14(6):94-100 (in Chinese with English abstract). [23] Wei, Z.H, Wei, X.F.2014.Comparision of Gas Bearing Property Between Different Pore Types of Shale:A Case from the Upper Ordovician Wufeng and Longmaxi Fms in the Jiaoshiba Area, Sichuan Basin.Natural Gas Industry, 34(6):37-41 (in Chinese with English abstract). https://www.researchgate.net/publication/286395667_Comparison_of_gas-bearing_property_between_different_pore_types_of_shale_A_case_from_the_Upper_Ordovician_Wufeng_and_Longmaxi_Fms_in_the_Jiaoshiba_area_Sichuan_Basin [24] Yan, D.P., Wang, X.W, Liu, Y.Y., 2000.Analysis of Fold Style and Its Formation Mechanism in the Area of Boundary among Sichuan, Hubei and Hunan.Geoscience, 14(1):37-43 (in Chinese with English abstract). https://www.researchgate.net/publication/307557663_Analysis_of_fold_style_and_its_formation_mechanism_in_the_area_of_boundary_among_Sichuan_Hubei_and_Hunan [25] Zhang, J.C., Jiang, S.L., Tang, X., et al., 2009.Accumulation Types and Resources Characteristics of Shale Gas in China.Natural Gas Industry, 29(12):109-114 (in Chinese with English abstract). [26] Zhang, J.C., Jin, Z.J., Yuan, M.S., 2004.Reservoiring Mechanism of Shale Gas and Its Distribution.Natural Gas Industry, 24(7):15-18 (in Chinese with English abstract). https://www.researchgate.net/publication/303636775_Reservoiring_mechanism_of_shale_gas_and_its_distribution [27] Zhang, J.C., Nie, H.K., Xu, B., et al., 2008.Geological Condition of Shale Gas Accumulation in Sichuan Basin.Natural Gas Industry, 28(2):151-156 (in Chinese with English abstract). [28] Zhang, M., Z., Peng, S.B., Zhang, L., et al., 2016.New Rocognition of Carbonate Nodules Genesis in Sinian Doushantuo Formation in Zigui Area and Its Geological Implication.Earth Science, 41(12):1977-1994 (in Chinese with English abstract). https://www.researchgate.net/publication/312128271_New_recognition_of_carbonate_nodules_genesis_in_sinian_doushantuo_formation_in_zigui_area_and_its_geological_implication [29] Zhang, X., Jiang, T.X., Jia, C.G., et al., 2013.Physical Simulation of Hydraulic Fracturing of Shale Gas Reservoir.Petroleum Drilling Techniques, 41(2):70-74 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYZT201302016.htm [30] Zhang, X.M., Shi, W.Z., Xu, Q.H., et al., 2015.Reservoir Characteristics and Controlling Factors of Shale Gas in Jiaoshiba Area, Sichuan Basin.Acta Petrolei Sinica, 36(8):926-939 (in Chinese with English abstract). https://www.researchgate.net/publication/283092654_Reservoir_characteristics_and_controlling_factors_of_shale_gas_in_Jiaoshiba_area_Sichuan_Basin [31] Zou, C.N., Dong, D.Z., Wang, S.J., et al., 2010.Geological Characteristics, Formation Mechanism and Resource Potential of Shale Gas in China.Petroleum Exploration and Development, 37(6):641-653 (in Chinese with English abstract). doi: 10.1016/S1876-3804(11)60001-3 [32] 陈尚斌, 朱炎铭, 王红岩, 等, 2011.四川盆地南缘下志留统龙马溪组页岩气储层矿物成分特征及意义.石油学报, 32(5): 775-782. doi: 10.7623/syxb201105006 [33] 董大忠, 程克明, 王玉满, 等, 2010.中国上扬子区下古生界页岩气形成条件及特征.石油与天然气地质, 31(3): 288-299, 308. doi: 10.11743/ogg20100304 [34] 关小旭, 伊向艺, 杨火海, 2014.中美页岩气储层条件对比.西南石油大学学报(自然科学版), 36(5): 33-39. doi: 10.11885/j.issn.1674-5086.2013.12.05.01 [35] 郭彤楼, 张汉荣, 2014.四川盆地焦石坝页岩气田形成与富集高产模式.石油勘探与开发, 41(1): 28-36. doi: 10.11698/PED.2014.01.03 [36] 郭旭升, 2014.南方海相页岩气"二元富集"规律——四川盆地及周缘龙马溪组页岩气勘探实践认识.地质学报, 88(7): 1209-1218. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201407001.htm [37] 郭旭升, 郭彤楼, 魏志红, 等, 2012.中国南方页岩气勘探评价的几点思考.中国工程科学, 14(6): 101-105, 112. http://www.cnki.com.cn/Article/CJFDTOTAL-GCKX201206013.htm [38] 胡东风, 张汉荣, 倪楷, 等, 2014.四川盆地东南缘海相页岩气保存条件及主控因素.天然气工业, 34(6): 17-23. http://www.cnki.com.cn/Article/CJFDTOTAL-TRQG201406003.htm [39] 蒋成平, 雷应金, 龚进, 等, 2011.页岩气成藏条件及我国页岩气分布与前景.内蒙古石油化工, 18: 133-135. doi: 10.3969/j.issn.1006-7981.2011.14.054 [40] 李欣, 段胜楷, 孙扬, 等, 2011.美国页岩气勘探开发最新进展.天然气工业, 31(8): 124-126. http://www.cnki.com.cn/Article/CJFDTOTAL-TRQG201108037.htm [41] 李新景, 胡素云, 程克明, 2007.北美裂缝性页岩气勘探开发的启示.石油勘探与开发, 34(4): 392-400. http://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200704003.htm [42] 李新景, 吕宗刚, 董大忠, 等, 2009.北美页岩气资源形成的地质条件.天然气工业, 29(5): 27-32. http://www.cnki.com.cn/Article/CJFDTOTAL-TRQG200905006.htm [43] 李湘涛, 石文睿, 郭美瑜, 等, 2014.涪陵页岩气田焦石坝区海相页岩气层特征研究.石油天然气学报, 36(11): 11-15. doi: 10.3969/j.issn.1000-9752.2014.11.004 [44] 梁狄刚, 郭彤楼, 陈建平, 等, 2009.中国南方海相生烃成藏研究的若干新进展(三)南方四套区域性海相烃源岩的沉积相及发育的控制因素.海相油气地质, 14(2): 1-19. http://www.cnki.com.cn/Article/CJFDTOTAL-HXYQ200902003.htm [45] 刘竞, 徐海棠, 余果, 等, 2014.四川盆地页岩气开发指标与开发潜力分析.天然气勘探与开发, 37(2): 45-47, 52. http://www.cnki.com.cn/Article/CJFDTOTAL-TRKT201402011.htm [46] 聂海宽, 唐玄, 边瑞康, 2009.页岩气成藏控制因素及中国南方页岩气发育有利区预测.石油学报, 30(4): 484-491. doi: 10.7623/syxb200904002 [47] 聂海宽, 张金川, 包书景, 等, 2012.四川盆地及其周缘上奥陶统-下志留统页岩气聚集条件.石油与天然气地质, 33(3): 335-345. doi: 10.11743/ogg20120302 [48] 谭淋耘, 徐铫, 李大华, 等, 2015.渝东南地区五峰组——龙马溪组页岩气成藏地质条件与有利区预测.地质学报, 89(7): 1308-1317. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201507013.htm [49] 王红岩, 郭伟, 梁峰, 等, 2015.四川盆地威远页岩气田五峰组和龙马溪组黑色页岩生物地层特征与意义.地层学杂志, 39(3): 289-293. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ201503006.htm [50] 王社教, 王兰生, 黄金亮, 等, 2009.上扬子区志留系页岩气成藏条件.天然气工业, 29(5): 45-50, 137. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201106012.htm [51] 王社教, 杨涛, 张国生, 等, 2012.页岩气主要富集因素与核心区选择及评价.中国工程科学, 14(6): 94-100. http://www.cnki.com.cn/Article/CJFDTOTAL-GCKX201206012.htm [52] 魏志红, 魏祥峰, 2014.页岩不同类型孔隙的含气性差异——以四川盆地焦石坝地区五峰组-龙马溪组为例.天然气工业, 34(6): 37-41. http://www.cnki.com.cn/Article/CJFDTOTAL-TRQG201406007.htm [53] 颜丹平, 汪新文, 刘友元, 2000.川鄂湘边区褶皱构造样式及其成因机制分析.现代地质, 14(1): 37-43. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ200001007.htm [54] 张金川, 姜生玲, 唐玄, 等, 2009.我国页岩气富集类型及资源特点.天然气工业, 29(12): 109-114. doi: 10.3787/j.issn.1000-0976.2009.12.033 [55] 张金川, 金之钧, 袁明生, 2004.页岩气成藏机理和分布.天然气工业, 24(7): 15-18. http://www.cnki.com.cn/Article/CJFDTOTAL-TRQG200407004.htm [56] 张金川, 聂海宽, 徐波, 等, 2008.四川盆地页岩气成藏地质条件.天然气工业, 28(2): 151-156. http://www.cnki.com.cn/Article/CJFDTOTAL-TRQG200802057.htm [57] 张明正, 彭松柏, 张利, 等, 2016.秭归地区震旦系陡山沱组碳酸盐岩结核成因新认识及其地质意义.地球科学, 41(12): 1977-1994. http://www.earth-science.net/WebPage/Article.aspx?id=3395 [58] 张旭, 蒋廷学, 贾长贵, 等, 2013.页岩气储层水力压裂物理模拟试验研究.石油钻探技术, 41(2): 70-74. http://cdmd.cnki.com.cn/Article/CDMD-10491-1014340965.htm [59] 张晓明, 石万忠, 徐清海, 等, 2015.四川盆地焦石坝地区页岩气储层特征及控制因素.石油学报, 36(8): 926-939. doi: 10.7623/syxb201508004 [60] 邹才能, 董大忠, 王社教, 等, 2010.中国页岩气形成机理、地质特征及资源潜力.石油勘探与开发, 37(6): 641-653. http://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201006003.htm -
点击查看大图
图(9) / 表(1)
计量
- 文章访问数: 4554
- HTML全文浏览量: 2463
- PDF下载量: 105
- 被引次数: 0
