Sedimentary characteristics and favourable area selection of tight sandstone gas reservoirs in the Sanjianfang Formation of the Shengbei Depression, Tuha Basin
-
摘要:
胜北凹陷是吐哈盆地最大的富油气洼陷, 随着对中侏罗统三间房组致密砂岩气勘探开发的需求强烈, 亟需对三间房组沉积特征进行研究, 预测有利勘探区带。通过岩心观察、测井和地震资料分析等手段, 结合高分辨率层序地层学对胜北凹陷中侏罗统三间房组致密砂岩气藏沉积特征进行研究, 建立三角洲-湖泊沉积体系, 预测了致密气藏有利勘探区带。吐哈盆地胜北凹陷三间房组发育3个长期层序(L1, L2, L3)和5个中期层序(M1, M2, M3, M4, M5), 中期旋回区域对比良好。M1~M3层序沉积期, 主要发育辫状河三角洲-湖泊沉积体系; M4~M5层序沉积期为曲流河三角洲-湖泊。胜北凹陷三间房组有利储层的砂体主要发育于三角洲前缘亚相。平面上M2层序沉积期胜北5井和胜深3井井区、M3层序沉积期胜北5井和胜北6井井区及东北部和M5层序沉积期胜北5井、胜北6井和胜探1井井区为有利勘探区, M4层序沉积期有利储层整体不发育。该研究成果对促进吐哈盆地胜北凹陷三间房组致密气藏勘探具有指导意义。
Abstract:Objective The Shengbei Depression is the largest petroliferous depression of the Tuha Basin. With the strong demand for the exploration and development of tight sandstone gas in the Middle Jurassic Sanjianfang Formation, it is urgent to study the sedimentary characteristics and predict favourable exploration zones of the Sanjianfang Formation.
Methods Using core, well logging, and seismic data, the high-resolution sequences and sedimentary characteristics of the tight sandstone gas reservoir in the Sanjianfang Formation of the Shengbei Depression were studied. A lacustrine delta system was identified, and favourable exploration zones of tight gas reservoirs were predicted.
Results Three long-term sequences (L1, L2, L3) and five medium-term sequences (M1, M2, M3, M4, M5) were developed in the Sanjianfang Formation in the Shengbei Depression; particularly, these medium-term sequences can be regionally identified. The deposition of the M1 to M3 sequences involved a braided river delta in the lake, but the deposition of the M4-M5 sequences involved a meandering river delta in the lake. The favourable tight gas reservoirs of the Sanjianfang Formation in the Shengbei Depression were mainly developed in subfacies of the delta front. On the plane, the Shengbei 5 and Shengshen 3 well areas of the M2 sequence, the Shengbei 5 and Shengbei 6 well areas of the M3 sequence, and the Shengbei 5, Shengbei 6, and Shengtan 1 well areas of the M5 sequence are favorable exploration areas. The favorable reservoir rarely appears in the M4 sequence.
Conclusion This research can promote the exploration of tight gas reservoirs in the Sanjianfang Formation of the Shengbei Depression in the Tuha Basin.
-
图 1 吐哈盆地胜北凹陷构造位置图
Figure 1. Structural location map of the Shengbei Depression in the Tuha Basin
图 2 胜北凹陷中侏罗统三间房组层序地层与沉积相综合柱状图
Figure 2. Sedimentary facies and stratigraphic sequence of the Middle Jurassic Sanjianfang Formation in the Shengbei Depression
图 3 胜北凹陷中侏罗统三间房组层序地层地层格架
Figure 3. Sequence stratigraphic framework of the Middle Jurassic Sanjianfang Formation in the Shengbei Depression
图 4 胜北凹陷中侏罗统三间房组连井相沉积相对比图
Figure 4. Comparison of sedimentary facies of the Middle Jurassic Sanjianfang Formation in the well cross-section of the Shengbei Depression
图 5 胜北凹陷中侏罗统三间房组M1层序沉积相图
Figure 5. Sedimentary facies of the M1 sequence of the Middle Jurassic Sanjianfang Formation in the Shengbei Depression
图 6 胜北凹陷中侏罗统三间房组M2层序沉积相图
Figure 6. Sedimentary facies of the M2 sequence of the Middle Jurassic Sanjianfang Formation in the Shengbei Depression
图 7 胜北凹陷中侏罗统三间房组M3层序沉积相图
Figure 7. Sedimentary facies of the M3 sequence of the Middle Jurassic Sanjianfang Formation in the Shengbei Depression
图 8 胜北凹陷中侏罗统三间房组M4层序沉积相图
Figure 8. Sedimentary facies of the M4 sequence of the Middle Jurassic Sanjianfang Formation in the Shengbei Depression
图 9 胜北凹陷中侏罗统三间房组M5层序沉积相图
Figure 9. Sedimentary facies of the M5 sequence of the Middle Jurassic Sanjianfang Formation in the Shengbei Depression
图 10 胜北凹陷三间房组有利区带综合评价图
Figure 10. Comprehensive evaluation of favourable zones in the Sanjianfang Formation of the Shengbei Depression
表 1 研究区中侏罗统主要沉积相类型
Table 1. Main sedimentary facies types of the Middle Jurassic in the study area
沉积体系 沉积相 亚 相 微 相 主要岩性组合 层位 三角洲体系 辫状河三角洲 三角洲前缘 水下分流河道、分流间湾 含砾砂岩和中、细砂岩及暗色泥岩 三间房组下部 前三角洲 前三角洲泥 粉砂岩、泥质粉砂岩、泥岩 曲流河三角洲 三角洲前缘 水下分流河道、分流间湾、河口坝 中、细砂岩及紫色泥岩 三间房组上部 前三角洲 前三角洲泥 粉砂岩、泥质粉砂岩、泥岩 湖泊体系 湖泊 (半)深湖 (半)深湖泥 暗色粉砂泥岩、暗色泥岩 七克台组 (极)浅湖 (极)浅湖泥、浅湖砂坝 粉砂质泥岩、暗色泥岩、紫色泥岩 
下载: 导出CSV
-
[1] 姚文礼. 四川盆地须家河组致密砂岩物源体系的控储作用[J]. 地质科技通报, 2021, 40(5): 223-230. doi: 10.19509/j.cnki.dzkq.2021.0036YAO W L. Reservoir control tight sandstone provenance system in the Xujiahe Formation, Sichuan Basin[J]. Bulletin of Geological Science and Technology, 2021, 40 (5): 223-230. (in Chinese with English abstract) doi: 10.19509/j.cnki.dzkq.2021.0036 [2] 彭伟, 舒逸, 陈绵琨, 等. 四川盆地复兴地区侏罗系凉高山组致密砂岩储层特征及其主控因素[J]. 地质科技通报, 2023, 42(3): 102-113. doi: 10.19509/j.cnki.dzkq.tb20220282PENG W, SHU Y, CHEN M K, et al. Tight sandstone reservoir characteristics and main controlling factors of Jurassic Lianggaoshan Formation in Fuxing area, Sichuan Basin[J]. Bulletin of Geological Science and Technology, 2023, 42(3): 102-113. (in Chinese with English abstract). doi: 10.19509/j.cnki.dzkq.tb20220282 [3] 陈淑鹏, 蔡苏阳, 梁云, 等. 吐哈盆地胜北凹陷中侏罗统致密砂岩储层孔隙发育特征及控制因素[J]. 地质科技通报, 2023, 42(3): 189-200. doi: 10.19509/j.cnki.dzkq.2022.0129CHEN S P, CAI S Y, LIANG Y, et al. Pore characteristics and its controlling factors in the Middle Jurassic tight sandstone reservoirs of the Shengbei Sag, Turpan-Hami Basin[J]. Bulletin of Geological Science and Technology, 2023, 42(3): 189-200. (in Chinese with English abstract) doi: 10.19509/j.cnki.dzkq.2022.0129 [4] 梁世君, 钱峰, 肖冬生. 吐哈盆地台北凹陷吉7H井侏罗系致密砂岩油气藏勘探发现与启示[J]. 中国石油勘探, 2022, 27(1): 50-59. doi: 10.3969/j.issn.1672-7703.2022.01.005LIANG S J, QIAN F, XIAO D S. Exploration discovery and implications of the Jurassic tight sandstone oil and gas reservoir in Well Ji7H in Taibei Sag, Turpan-Hami Basin[J]. China Petroleum Exploration, 2022, 27(1): 50-59. (in Chinese with English abstract) doi: 10.3969/j.issn.1672-7703.2022.01.005 [5] 苟红光, 张品, 佘家朝, 等. 吐哈盆地石油地质条件、资源潜力及勘探方向[J]. 海相油气地质, 2019, 24(2): 85-96. doi: 10.3969/j.issn.1672-9854.2019.02.009GOU H G, ZHANG P, SHE J C, et al. Petroleum geological conditions, resource potential and exploration direction in Turpan-Hami Basin[J]. Marine Origin Petroleum Geology, 2019, 24(2): 85-96. (in Chinese with English abstract) doi: 10.3969/j.issn.1672-9854.2019.02.009 [6] 梁世君. 吐哈探区油气勘探成果及潜力[J]. 新疆石油地质, 2020, 41(6): 631-641. https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD202006002.htmLIANG S J. Achievements and potential of petroleum exploration in Tuha oil and gas province[J]. Xinjiang Petroleum Geology, 2020, 41(6): 631-641. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD202006002.htm [7] 袁明生, 梁世君, 燕列灿, 等. 吐哈盆地油气地质与勘探实践[M]. 北京: 石油工业出版社, 2002.YUAN M S, LIANG S J, YAN L C, et al. Petroleum geology and exploration in Turpan-Hami Basin[M]. Beijing: Petroleum Industry Press, 2002. (in Chinese with English abstract) [8] 袁明生. 吐哈盆地油气分布特征及勘探方向[J]. 新疆石油地质, 1998, 19(2): 106-111. https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD802.002.htmYUAN M S. Oil & gas distribution characteristics and exploration strategy in Turpan-Hami Basin[J]. Xinjiang Petroleum Geology, 1998, 19(2): 106-111. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD802.002.htm [9] 李文厚, 周立发, 柳益群, 等. 吐哈盆地沉积格局与沉积环境的演变[J]. 新疆石油地质, 1997, 18(2): 135-141. https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD199702008.htmLI W H, ZHOU L F, LIU Y Q, et al. Evolution of sedimentary framework and environment of Turpan-Hami Basin[J]. Xinjiang Petroleum Geology, 1997, 18(2): 135-141. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD199702008.htm [10] 郭威. 新疆博格达山及其邻区板内构造作用研究[D]. 西安: 西北大学, 2008.GUO W. Intraplate tectonics of Bogda Mountain in Xinjiang and its adjacent plates[D]. Xi'an: Northwest University, 2008. (in Chinese with English abstract) [11] 肖冬生, 陈旋, 康积伦, 等. 博格达山构造演化对吐哈盆地台北凹陷西缘油气成藏的控制作用[J]. 中南大学学报(自然科学版), 2014, 45(11): 3877-3885. https://www.cnki.com.cn/Article/CJFDTOTAL-ZNGD201411022.htmXIAO D S, CHEN X, KANG J L, et al. Controlling functions of tectonic evolution of Bogeda Mountain on petroleum accumulation in western Taibei Sag, Turpan-Hami Basin[J]. Journal of Central South University (Science and Technology Edition), 2014, 45(11): 3877-3885. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-ZNGD201411022.htm [12] 郑荣才, 彭军, 吴朝容. 陆相盆地基准面旋回的级次划分和研究意义[J]. 沉积学报, 2001, 19(2): 249-255. doi: 10.3969/j.issn.1000-0550.2001.02.015ZHENG R C, PENG J, WU C R. Grade division of base-level cycles of terrigenous basin and its implications[J]. Acta Sedimentologica Sinica, 2001, 19(2): 249-255. (in Chinese with English abstract) doi: 10.3969/j.issn.1000-0550.2001.02.015 [13] 郑荣才, 吴朝容, 叶茂才. 浅谈陆相盆地高分辨率层序地层研究思路[J]. 成都理工学院学报, 2000, 27(3): 241-244. doi: 10.3969/j.issn.1671-9727.2000.03.005ZHENG R C, WU C R, YE M C. Research thinking of high-resolution sequence stratigraphy about a terrigenous basin[J]. Journal of Chengdu University of Technology, 2000, 27(3): 241-244. (in Chinese with English abstract) doi: 10.3969/j.issn.1671-9727.2000.03.005 [14] 邓宏文. 美国层序地层研究中的新学派: 高分辨率层序地层学[J]. 石油与天然气地质, 1995, 16(2): 89-97. doi: 10.3321/j.issn:0253-9985.1995.02.012DENG H W. A new school of thought in sequence stratigraphic studies in U.S.: High-resolution sequence stratigraphy[J]. Oil & Gas Geology, 1995, 16(2): 89-97. (in Chinese with English abstract) doi: 10.3321/j.issn:0253-9985.1995.02.012 [15] 马永生, 牟传龙, 郭彤楼, 等. 四川盆地东北部长兴组层序地层与储层分布[J]. 地学前缘, 2005, 12(3): 179-185. doi: 10.3321/j.issn:1005-2321.2005.03.019MA Y S, MU C L, GUO T L, et al. Sequence stratigraphy and reservoir distribution of the Changxing Formation in northeastern Sichuan Basin[J]. Earth Science Frontiers, 2005, 12(3): 179-185. (in Chinese with English abstract) doi: 10.3321/j.issn:1005-2321.2005.03.019 [16] 李国新, 徐胜林, 陈洪德, 等. 川西坳陷中段中侏罗统上沙溪庙组层序岩相古地理及砂体展布特征[J]. 中国地质, 2012, 39(1): 96-105. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201201011.htmLI G X, XU S L, CHEN H D, et al. Sedimentary facies and sand body distribution of the Middle Jurassic Upper Shaximiao Formation in the middle segment of western Sichuan Depression[J]. Geology in Chinese, 2012, 39(1): 96-105. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201201011.htm [17] 郑荣才, 戴朝成, 朱如凯, 等. 四川类前陆盆地须家河组层序-岩相古地理特征[J]. 地质论评, 2009, 55(4): 484-495. doi: 10.3321/j.issn:0371-5736.2009.04.003ZHENG R C, DAI C C, ZHU R K, et al. Sequence-based lithofacies and paleogeographic characteristics of Upper Triassic Xujiahe Formation in Sichuan Basin[J]. Geological Review, 2009, 55(4): 484-495. (in Chinese with English abstract) doi: 10.3321/j.issn:0371-5736.2009.04.003 [18] 李国新, 徐胜林, 陈洪德, 等. 鄂尔多斯盆地富县地区上三叠统长6段砂体展布规律研究[J]. 中国地质, 2012, 39(4): 923-930. doi: 10.3969/j.issn.1000-3657.2012.04.007LI G X, XU S L, CHEN H D, et al. The distribution regularity of sand bodies in Chang-6 Member of Upper Triassic Yanchang Formation, Fuxian area, Ordos Basin[J]. Geology in China, 2012, 39(4): 923-930. (in Chinese with English abstract) doi: 10.3969/j.issn.1000-3657.2012.04.007 [19] 李文厚, 柳益群, 冯乔, 等. 吐哈盆地侏罗系沉积相带与砂体的展布特征[J]. 石油实验地质, 1997, 19 (2): 168-172. https://www.cnki.com.cn/Article/CJFDTOTAL-SYSD199702011.htmLI W H, LIU Y Q, FENG Q, et al. Distributing characteristics of sedimentary facies belts and sandstone bodies of Jurassic in Turpan-Hami Basin[J]. Experimental Petroleum Geology, 1997, 19(2): 168-172. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-SYSD199702011.htm [20] 李文厚, 柳益群, 冯乔, 等. 台北凹陷中侏罗统辫状河三角洲沉积体系与油气的关系[J]. 西北大学学报(自然科学版), 1997, 27 (3): 247-252. doi: 10.3321/j.issn:1000-274X.1997.03.003LI W H, LIU Y Q, FENG Q, et al. The relations between barid river deltas depositional system and hydrocarbon resources in Taibei Sag[J]. Journal of Northwest University (Natural Science Edition), 1997, 27(3): 247-252. (in Chinese with English abstract) doi: 10.3321/j.issn:1000-274X.1997.03.003 [21] 刘林玉, 柳益群, 李文厚, 等. 吐哈盆地台北凹陷三角洲沉积与成岩作用[J]. 石油与天然气地质, 2002, 23(4): 402-405. doi: 10.3321/j.issn:0253-9985.2002.04.021LIU L Y, LIU Y Q, LI W H, et al. Sedimentation and diagenesis of delta in Taibei Sag of Turfan-Hami Basin[J]. Oil & Gas Geology, 2002, 23(4): 402-405. (in Chinese with English abstract) doi: 10.3321/j.issn:0253-9985.2002.04.021 [22] 罗权生. 吐哈盆地神泉油田三间房组沉积微相特征[J]. 新疆石油地质, 2001, 22(4): 309-312. doi: 10.3969/j.issn.1001-3873.2001.04.012LUO Q S. Gas-oil accumulation and depositional microfacies characteristics of Sanjianfang Formation in Shengquan Oilfield of Turpan-Hami Basin[J]. Xinjiang Petroleum Geology, 2001, 22(4): 309-312. (in Chinese with English abstract) doi: 10.3969/j.issn.1001-3873.2001.04.012 [23] 肖冬生, 杨占龙. 吐哈盆地台北凹陷西缘油气成藏过程主控因素及成藏模式[J]. 中南大学学报(自然科学版), 2013, 44(2): 679-686. https://www.cnki.com.cn/Article/CJFDTOTAL-ZNGD201302036.htmXIAO D S, YANG Z L. Controlling factors and accumulation model of hydrocarbon accumulation in western Taibei Sag, Turpan-Hami Basin[J]. Journal of Central South University (Science and Technology Edition), 2013, 44(2): 679-686. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-ZNGD201302036.htm [24] 曲丽丽, 段健, 余成林, 等. 辫状河三角洲前缘水下分流河道精细刻画方法: 以南堡凹陷M油田东一段为例[J]. 地质科技通报, 2023, 42(3): 134-141. doi: 10.19509/j.cnki.dzkq.tb20220645QU L L, DUAN J, YU C L, et al. Fine description method of the underwater distributary channel in a braided river delta front: A case study of the first Member of the Dongying Formation in the M Oilfield, Nanpu Depression[J]. Bulletin of Geological Science and Technology, 2023, 42(3): 134-141. (in Chinese with English abstract) doi: 10.19509/j.cnki.dzkq.tb20220645 -
下载:
点击查看大图
计量
- 文章访问数: 274
- PDF下载量: 90
- 被引次数: 0
