Fracture characteristics and hydrocarbon significance in the Chang 7 to Chang 9 members of Triassic Yanchang Formation of Gufengzhuang area, western Ordos Basin
-
摘要: 天然裂缝对鄂尔多斯盆地三叠系延长组低渗透油藏的勘探开发具有重要的作用。盆地古峰庄地区延长组油气资源丰富，具有良好的勘探前景，但有关裂缝研究成果较少，对其分布规律和活动时期认识不清。通过古峰庄地区延长组长7—长9段岩心、成像测井、碳—氧同位素、流体包裹体、岩石声发射及构造应力和断裂活动分析，对其天然裂缝的特征、形成期次及成因进行研究，并探讨了裂缝对油气成藏的作用。古峰庄地区长7—长9段天然裂缝较发育，尤以长7段最发育；以高角度和垂直裂缝为主，走向以NEE向为主，NE向次之，少量NW和NWW向；裂缝以未充填和方解石半充填为主，有效性较好；裂缝面较平直，可见油侵、油迹、油斑等明显的油气运移痕迹。长7、长8、长9段氧同位素均值分别为-15.8‰，-17.5‰，-18.7‰，裂缝的形成深度分别为1 675，2 338，2 785 m；由流体包裹体均一温度峰值90~100 ℃，120~130 ℃，换算得裂缝形成深度范围在1 750~2 000 m，2 500~2 750 m。该区长7—长9段裂缝活动具有多期性，可划分为印支期、燕山期和喜马拉雅期，燕山期和喜马拉雅期为主要活动时期。不同时期发育的有效性裂缝改善了研究区低渗透储层的物性，为长7—长9段等多层系—深层系油藏的形成提供了重要运移通道和储集空间，并影响着油井的产能。Abstract: Natural fractures play an important role for the exploration and development of low-permeability reservoirs in the Triassic Yanchang Formation of the Ordos Basin. Abundant hydrocarbon resources have been found in the Yanchang Formation of the Gufengzhuang area, showing good exploration prospects. However, only limited research results on fractures have been obtained, and the distribution law and active period are both unclear. Based on the analyses of core, imaging logging, carbon-oxygen isotope, homogenization temperature of fluid inclusion, acoustic emission, tectonic stress and fracture activity, the characteristics, formation stages and causes of natural fractures in the Chang 7 to Chang 9 members of the Yanchang Formation in the Gufengzhuang area were studied, and corresponding indications for petroleum accumulation were discussed. Natural fractures are well-developed in the Chang 7 to Chang 9 members of the Yanchang Formation, especially in the Chang 7 member. High-angle and vertical fractures are ubiquitously developed, mainly of NEE orientation, followed by NE, and finally NW and NWW. The fractures are generally unfilled or semi-filled by calcites, providing effective pathways for hydrocarbon migration. The fracture surface is flat, and obvious traces of oil migration such as oil invasion, oil stain and oil spot can be observed. The average values of oxygen isotopes of the Chang 7 to Chang 9 members are -15.8‰, -17.5‰ and -18.7‰, indicating that the factures were formed at depth of 1 675, 2 338 and 2 785 m. According to the homogenization temperature peaks of fluid inclusions of 90-100 ℃ and 120-130 ℃, the formation depth of fractures is 1 750-2 000 m and 2 500-2 750 m. The fractures in the Chang 7 to Chang 9 members were active during multiple stages, including the Indosinian, Yanshanian and Himalayan stages, with the Yanshanian and Himalayan as the main active stages. Effective fractures developed in multiple stages have improved the physical properties of low-permeability reservoirs in the study area. They provided important migration channels and storage spaces for the formation of multi-layer and deep-layer reservoirs such as Chang 7, Chang 8 and Chang 9, and affected the productivity of oil wells.
-
图 1 鄂尔多斯盆地西部古峰庄地区构造位置及其三叠系延长组地层综合柱状图
Figure 1. Structural location of Gufengzhuang area in western Ordos Basin and comprehensive stratigraphic histogram of Triassic Yanchang Formation
图 2 鄂尔多斯盆地西部古峰庄地区延长组长7—长9段裂缝特征
a.F34井，长7段，2 321.64 m，裂缝方解石脉体填充，油斑；b.Y156井，长7段，2 200.5 m，裂缝，油迹；c.Y125井，长8段，2 420.1 m，裂缝见明显油气运移痕迹；d.Y120井，长9段，裂缝，无充填；e.Y120井，长9段，1 677.2 m，裂缝方解石脉体半充填；f.F2井，长8段，2 390.4 m，扫描电镜，微裂缝；g.F34井，长9段，2 490 m，扫描电镜，微裂缝；h.F21井，长8段，2 443.47 m，荧光，微裂缝
Figure 2. Characteristics of fractures in Chang 7 to Chang 9 members of Triassic Yanchang Formation, Gufengzhuang area, western Ordos Basin
图 3 鄂尔多斯盆地西部古峰庄地区延长组长7—长9段裂缝充填类型
Figure 3. Filling types of fractures in Chang 7 to Chang 9 members of Triassic Yanchang Formation, Gufengzhuang area, western Ordos Basin
图 4 鄂尔多斯盆地西部古峰庄地区长7段—长9段成像测井天然裂缝特征
Figure 4. Image logging showing characteristics of natural fractures in Chang 7 to Chang 9 members of Triassic Yanchang Formation, Gufengzhuang area, western Ordos Basin
图 5 鄂尔多斯盆地西部古峰庄地区延长组长7—长9段裂缝产状特征
Figure 5. Occurrence of fractures in Chang 7 to Chang 9 members of Triassic Yanchang Formation, Gufengzhuang area, western Ordos Basin
图 6 鄂尔多斯盆地西部古峰庄地区延长组长7—长9段裂缝平面展布(a-c)及其与断裂关系(d)
Figure 6. Plane distribution (a-c) and their relationship with faults (d) of fractures in Chang 7 to Chang 9 members of Triassic Yanchang Formation, Gufengzhuang area, western Ordos Basin
图 7 鄂尔多斯盆地西部古峰庄地区延长组长7—长9段裂缝充填物形成时期
Figure 7. Formation period of fillings in fractures in Chang 7 to Chang 9 members of Triassic Yanchang Formation, Gufengzhuang area, western Ordos Basin
图 8 鄂尔多斯盆地西部古峰庄地区不同时期断裂活动特征解释结果
Figure 8. Interpretation of fault activities in different periods in Gufengzhuang area, western Ordos Basin
图 9 鄂尔多斯盆地西部古峰庄地区断裂/裂缝形成示意
Figure 9. Formation of faults and fractures in Gufengzhuang area, western Ordos Basin
图 10 鄂尔多斯盆地西部古峰庄地区典型井三叠系延长组长9段综合评价
Figure 10. Comprehensive evaluation of Chang 9 member of Triassic Yanchang Formation in typical wells, Gufengzhuang area, western Ordos Basin
表 1 鄂尔多斯盆地西部古峰庄地区裂缝与储层物性、单井产量关系
Table 1. Physical properties of fractures and reservoirs vs. single well productions, Gufengzhuang area, western Ordos Basin
井位 层位 无裂缝发育段 裂缝发育段 裂缝发育密度/(条·m-1) 裂缝产状 产量/(t·d-1) 平均孔隙度/% 平均渗透率/10-3 μm2 平均孔隙度/% 平均渗透率/10-3 μm2 走向 裂缝角度 F21 长9 8.95 0.36 15.55 6.59 0.50 1条NE、1条NEE 皆为垂直开启裂缝 121.72 F34 长9 12.03 0.72 15.43 1.97 0.43 1条NW、2条NEE NW向为高角度闭合裂缝、NEE为垂直开启裂缝 56.27 Y65 长7 4.42 0.03 10.09 0.15 0.57 3条NEE、1条NWW 皆为垂直开启裂缝 6.46 Y155 长8 10.07 0.37 15.10 0.80 0.08 1条NEE 高角度开启裂缝 4.42 Y373 长9 9.34 0.24 13.98 1.40 0.26 4条NEE 3条为垂直开启裂缝、1条为高角度开启裂缝 产水 Y377 长9 9.85 0.30 11.69 0.64 0.25 2条NE、1条NEE NE向为垂直开启裂缝、NEE为高角度开启裂缝 产水 
下载: 导出CSV
-
[1] DENG Ben, ZHAO Hong, QU Mengmeng, et al. Distribution characteristics, genesis analyses, and research significance of Triassic regional structural fractures in the Ordos Basin, central China[J]. Geological Journal, 2018, 53(S1): 212-224. doi: 10.1002/gj.3165/abstract [2] 夏东领, 伍岳, 夏冬冬, 等. 鄂尔多斯盆地南缘红河油田长8致密油藏非均质性表征方法[J]. 石油实验地质, 2021, 43(4): 704-712. doi: 10.11781/sysydz202104704XIA Dongling, WU Yue, XIA Dongdong, et al. Characterization method of heterogeneity for Chang 8 tight reservoir in Honghe oil field, southern margin of Ordos Basin[J]. Petroleum Geology & Experiment, 2021, 43(4): 704-712. doi: 10.11781/sysydz202104704 [3] 王启宇, 郑荣才, 梁晓伟, 等. 鄂尔多斯盆地姬塬地区延长组裂缝特征及成因[J]. 成都理工大学学报(自然科学版), 2011, 38(2): 220-228. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG201102016.htmWANG Qiyu, ZHENG Rongcai, LIANG Xiaowei, et al. Feature and genesis of the reservoir fractures of Upper Triassic Yanchang Formation in Jiyuan area, Ordos Basin[J]. Journal of Chengdu University of Technology (Science & Technology Edition), 2011, 38(2): 220-228. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG201102016.htm [4] FAN Jianming, QU Xuefeng, WANG Chong, et al. Natural fracture distribution and a new method predicting effective fractures in tight oil reservoirs in Ordos Basin, NW China[J]. Petroleum Exploration and Development, 2016, 43(5): 806-814. doi: 10.1016/S1876-3804(16)30096-9 [5] 刘行军, 杨双定, 谢刚, 等. 鄂尔多斯盆地合水地区长8段裂缝发育特征及其对产油量的影响[J]. 油气地质与采收率, 2014, 21(6): 57-60. doi: 10.3969/j.issn.1009-9603.2014.06.014LIU Xingjun, YANG Shuangding, XIE Gang, et al. The study of relationship between fracture characteristic and yield of Chang8 section in Heshui area, Ordos Basin[J]. Petroleum Geology and Recovery Efficiency, 2014, 21(6): 57-60. doi: 10.3969/j.issn.1009-9603.2014.06.014 [6] 曾联波. 低渗透砂岩油气储层裂缝及其渗流特征[J]. 地质科学, 2004, 39(1): 11-17. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200401001.htmZENG Lianbo. Fissure and its seepage Characteristics in low-permeable sandstone reservoir[J]. Chinese Journal of Geology, 2004, 39(1): 11-17. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200401001.htm [7] 付金华. 科学出版社·地质分社图书推荐《鄂尔多斯盆地致密油勘探理论与技术》[J]. 中国科学: 地球科学, 2018, 48(6): 811. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201806014.htmFU Jinhua. Exploration theory and technology of tight oil in Ordos Basin[J]. Chinese Science: Earth Science, 2018, 48(6): 811. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201806014.htm [8] 马海勇, 周立发, 张雪峰, 等. 陕西省定边—吴起地区延长组长8地层裂缝形成因素分析[J]. 陕西师范大学学报(自然科学版), 2016, 44(2): 106-110. https://www.cnki.com.cn/Article/CJFDTOTAL-SXSZ201602020.htmMA Haiyong, ZHOU Lifa, ZHANG Xuefeng, et al. Analysis of factors affecting fractures of Chang-8 subsection based on Dingbian-Wuqi area of Shaanxi Province[J]. Journal of Shaanxi Normal University (Natural Science Edition), 2016, 44(2): 106-110. https://www.cnki.com.cn/Article/CJFDTOTAL-SXSZ201602020.htm [9] 赵向原, 曾联波, 王晓东, 等. 鄂尔多斯盆地宁县—合水地区长6、长7、长8储层裂缝差异性及开发意义[J]. 地质科学, 2015, 50(1): 274-285. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX201501018.htmZHAO Xiangyuan, ZENG Lianbo, WANG Xiaodong, et al. Differences of natural fracture characteristics and their development significance in Chang 6, Chang 7 and Chang 8 reservoir, Ningxian-Heshui area, Ordos Basin[J]. Chinese Journal of Geology, 2015, 50(1): 274-285. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX201501018.htm [10] 肖承钰, 尹伟, 张颖, 等. 鄂尔多斯镇泾地区延长组成藏体系与油气富集模式[J]. 石油实验地质, 2015, 37(3): 347-353. doi: 10.11781/sysydz201503347XIAO Chengyu, YIN Wei, ZHANG Ying, et al. Petroleum accumulation systems and oil enrichment patterns of Yanchang Formation in Zhenjing area, southern Ordos Basin[J]. Petroleum Geology & Experiment, 2015, 37(3): 347-353. doi: 10.11781/sysydz201503347 [11] 邓虎成, 周文, 彭军, 等. 鄂尔多斯麻黄山地区裂缝与油气成藏关系[J]. 新疆地质, 2010, 28(1): 81-85. https://www.cnki.com.cn/Article/CJFDTOTAL-XJDI201001019.htmDENG Hucheng, ZHOU Wen, PENG Jun, et al. Relationship between fracture and hydrocarbon accumulation of Mahuangshan area in Ordos Basin[J]. Xinjiang Geology, 2010, 28(1): 81-85. https://www.cnki.com.cn/Article/CJFDTOTAL-XJDI201001019.htm [12] 梁晓伟, 韩永林, 王海红, 等. 鄂尔多斯盆地姬塬地区上三叠统延长组裂缝特征及其地质意义[J]. 岩性油气藏, 2009, 21(2): 49-53. https://www.cnki.com.cn/Article/CJFDTOTAL-YANX200902012.htmLIANG Xiaowei, HAN Yonglin, WANG Haihong, et al. Fracture characteristics and geological significance of Upper Triassic Yanchang Formation in Jiyuan area, Ordos Basin[J]. Lithologic Reservoirs, 2009, 21(2): 49-53. https://www.cnki.com.cn/Article/CJFDTOTAL-YANX200902012.htm [13] 高金栋. 鄂尔多斯盆地姬塬油田三叠系延长组长7油层组致密砂岩天然裂缝识别与建模[D]. 西安: 西北大学, 2018.GAO Jindong. Identification and modeling of tight sandstone natural fractures in Chang 7 section of Triassic Yanchang Formation in Jiyuan Oilfield, Ordos Basin[D]. Xi'an: Northwest University, 2018. [14] 李士祥, 邓秀芹, 庞锦莲, 等. 鄂尔多斯盆地中生界油气成藏与构造运动的关系[J]. 沉积学报, 2010, 28(4): 798-807. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201004019.htmLI Shixiang, DENG Xiuqin, PANG Jinlian, et al. Relationship between petroleum accumulation of Mesozoic and tectonic movement in Ordos Basin[J]. Acta Sedimentologica Sinica, 2010, 28(4): 798-807. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201004019.htm [15] 邵晓州, 王苗苗, 惠潇, 等. 鄂尔多斯盆地盐池地区裂缝特征、形成期次及发育模式[J]. 天然气地球科学, 2021, 32(10): 1501-1513. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202110007.htmSHAO Xiaozhou, WANG Miaomao, HUI Xiao, et al. Characteristics, formation stages and development model of fractures in Yanchi area, Ordos Basin[J]. Natural Gas Geoscience, 2021, 32(10): 1501-1513. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202110007.htm [16] 姜琳, 邱振, 郭玉森, 等. 鄂尔多斯盆地延长组次生矿物与裂缝形成时限分析[J]. 地质科学, 2017, 52(3): 915-930.JIANG Lin, QIU Zhen, GUO Yusen, et al. The analysis of secondary minerals and fracture formation time in Yanchang Formation of Ordos Basin[J]. Chinese Journal of Geology, 2017, 52(3): 915-930. [17] 邓虎成, 周文, 姜文利, 等. 鄂尔多斯盆地麻黄山西区块延长、延安组裂缝成因及期次[J]. 吉林大学学报(地球科学版), 2009, 39(5): 811-817. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200905008.htmDENG Hucheng, ZHOU Wen, JIANG Wenli, et al. Genetic mechanism and development periods of fracture in Yanchang and Yan'an formation of western Mahuangshan block in Ordos Basin[J]. Journal of Jilin University (Earth Science Edition), 2009, 39(5): 811-817. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200905008.htm [18] 王翠丽, 周文, 李红波, 等. 镇泾地区延长组多期次裂缝发育特征及分布[J]. 成都理工大学学报(自然科学版), 2014, 41(5): 596-603. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG201405009.htmWANG Cuili, ZHOU Wen, LI Hongbo, et al. Characteristics and distribution of multiphase fractures in Yanchang Formation of Zhenjing block in Ordos Basin, China[J]. Journal of Chengdu University of Technology (Science & Technology Edition), 2014, 41(5): 596-603. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG201405009.htm [19] 郑荣才. 储层裂缝研究的新方法—声发射实验[J]. 石油与天然气地质, 1998, 19(3): 186-189. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT803.002.htmZHENG Rongcai. A new method of studying reservoir fractures: acoustic emission experiment[J]. Oil & Gas Geology, 1998, 19(3): 186-189. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT803.002.htm [20] DONG Shaoqun, ZENG Lianbo, LYU Wenya, et al. Fracture identification by semi-supervised learning using conventional logs in tight sandstones of Ordos Basin, China[J]. Journal of Natural Gas Science and Engineering, 2020, 76: 103131. http://www.sciencedirect.com/science/article/pii/S187551001930383X [21] LOHR T, KRAWCZYK C M, TANNER D C, et al. Strain partitioning due to salt: insights from interpretation of a 3D seismic data set in the NW German Basin[J]. Basin Research, 2007, 19(4): 579-597. doi: 10.1111/j.1365-2117.2007.00338.x/pdf [22] 朱兰, 李素华, 余洋, 等. 川西新场地区中三叠统雷口坡组顶部风化壳裂缝分布特征及预测[J]. 石油实验地质, 2022, 44(3): 448-455. doi: 10.11781/sysydz202203448ZHU Lan, LI Suhua, YU Yang, et al. Fracture distribution and prediction of weathering crust reservoirs on the top of Leikoupo Formation, Xinchang area, western Sichuan Basin[J]. Petroleum Geology & Experiment, 2022, 44(3): 448-455. doi: 10.11781/sysydz202203448 [23] 付金华, 李士祥, 刘显阳, 等. 鄂尔多斯盆地姬塬大油田多层系复合成藏机理及勘探意义[J]. 中国石油勘探, 2013, 18(5): 1-9. https://www.cnki.com.cn/Article/CJFDTOTAL-KTSY201305001.htmFU Jinhua, LI Shixiang, LIU Xianyang, et al. Multi-layer composite accumulation mechanism and exploration significance of Jiyuan Oilfield, Ordos Basin[J]. China Petroleum Exploration, 2013, 18(5): 1-9. https://www.cnki.com.cn/Article/CJFDTOTAL-KTSY201305001.htm [24] 曾联波, 李忠兴, 史成恩, 等. 鄂尔多斯盆地上三叠统延长组特低渗透砂岩储层裂缝特征及成因[J]. 地质学报, 2007, 81(2): 174-180. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200702005.htmZENG Lianbo, LI Zhongxing, SHI Cheng'en, et al. Characteristics and origin of fractures in the extra low-permeability sandstone reservoirs of the Upper Triassic Yanchang Formation in the Ordos Basin[J]. Acta Geologica Sinica, 2007, 81(2): 174-180. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200702005.htm [25] 周新桂, 张林炎, 范昆. 含油气盆地低渗透储层构造裂缝定量预测方法和实例[J]. 天然气地球科学, 2007, 18(3): 328-333. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX200703001.htmZHOU Xingui, ZHANG Linyan, FAN Kun. Methods for quantitative prediction of tectonic fractures in compact reservoirs in petroliferous basins and a case study[J]. Natural Gas Geoscience, 2007, 18(3): 328-333. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX200703001.htm [26] 张莉. 陕甘宁盆地储层裂缝特征及形成的构造应力场分析[J]. 地质科技情报, 2003, 22(2): 21-24. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200302005.htmZHANG Li. Characteristics of reservoir fracture and the analysis of stress field in Shaanxi-Gansu-Ningxia Basin[J]. Geological Science and Technology Information, 2003, 22(2): 21-24. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200302005.htm [27] 刘池洋, 赵红格, 桂小军, 等. 鄂尔多斯盆地演化—改造的时空坐标及其成藏(矿)响应[J]. 地质学报, 2006, 80(5): 617-638. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200605003.htmLIU Chiyang, ZHAO Hongge, GUI Xiaojun, et al. Space-time coordinate of the evolution and reformation and mineralization response in Ordos Basin[J]. Acta Geologica Sinica, 2006, 80(5): 617-638. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200605003.htm [28] 王允诚. 裂缝性致密油气储集层[M]. 北京: 地质出版社, 1992.WANG Yuncheng. Fractured tight oil and gas reservoir[M]. Beijing: Geological Publishing House, 1992. [29] EPSTEIN S, BUCHSBAUM R, LOWENSTAM H A, et al. Revised carbonate-water isotopic temperature scale[J]. GSA Bulletin, 1953, 64(11): 1315-1325. http://faculty.washington.edu/stn/ess_501/reading/Epstein_paleotemperatures_GSABull_1951.pdf [30] 郭凯, 曾溅辉, 李元昊, 等. 陇东地区延长组构造裂缝方解石脉特征及其与烃类流体活动的关系[J]. 中国石油大学学报(自然科学版), 2013, 37(2): 36-42. https://www.cnki.com.cn/Article/CJFDTOTAL-SYDX201302008.htmGUO Kai, ZENG Jianhui, LI Yuanhao, et al. Geochemical characte-ristics of tectonic fracture-filling calcite in Yanchang Formation of Longdong area and its relationship with hydrocarbon fluid flow[J]. Journal of China University of Petroleum, 2013, 37(2): 36-42. https://www.cnki.com.cn/Article/CJFDTOTAL-SYDX201302008.htm [31] 任战利, 于强, 崔军平, 等. 鄂尔多斯盆地热演化史及其对油气的控制作用[J]. 地学前缘, 2017, 24(3): 137-148. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201703016.htmREN Zhanli, YU Qiang, CUI Junping, et al. Thermal history and its controls on oil and gas of the Ordos Basin[J]. Earth Science Frontiers, 2017, 24(3): 137-148. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201703016.htm [32] 时保宏, 张艳, 张雷, 等. 鄂尔多斯盆地延长组长7致密储层流体包裹体特征与成藏期次[J]. 石油实验地质, 2012, 34(6): 599-603. doi: 10.11781/sysydz201206599SHI Baohong, ZHANG Yan, ZHANG Lei, et al. Hydrocarbon accumulation dating by fluid inclusion characteristics in Chang7 tight sandstone reservoirs of Yanchang Formation in Ordos Basin[J]. Petroleum Experimental Geology, 2012, 34(6): 599-603. doi: 10.11781/sysydz201206599 [33] 陈瑞银, 罗晓容, 赵文智, 等. 鄂尔多斯盆地中生代热异常及烃源岩热演化特征[J]. 石油勘探与开发, 2007, 34(6): 658-663. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200706005.htmCHEN Ruiyin, LUO Xiaorong, ZHAO Wenzhi, et al. Thermal anomaly and thermal evolution of source rocks in Mesozoic, Ordos Basin[J]. Petroleum Exploration and Development, 2007, 34(6): 658-663. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200706005.htm [34] 谷阳, 徐晟, 张炜, 等. 黔北地区龙马溪组页岩裂缝发育特征及地质意义[J]. 断块油气田, 2021, 28(6): 733-738. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT202106004.htmGU Yang, XU Sheng, ZHANG Wei, et al. Fracture development characteristics and geological significance of Longmaxi Formation shale in northern Guizhou[J]. Fault-Block Oil and Gas Field, 2021, 28(6): 733-738. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT202106004.htm [35] 彭先锋, 邓虎成, 何建华, 等. 鄂尔多斯盆地大牛地气田中奥陶统马家沟组裂缝特征及成因[J]. 石油实验地质, 2022, 44(1): 41-50. doi: 10.11781/sysydz202201041PENG Xianfeng, DENG Hucheng, HE Jianhua, et al. Characte-ristics and genesis of fractures in Middle Ordovician Majiagou Formation, Daniudi Gas Field, Ordos Basin[J]. Petroleum Geo-logy & Experiment, 2022, 44(1): 41-50. doi: 10.11781/sysydz202201041 [36] 尚墨翰, 赵向原, 胡向阳, 等. 川东北元坝地区陆相储层天然裂缝发育特征及分布模式[J]. 断块油气田, 2022, 29(1): 8-13. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT202201002.htmSHANG Mohan, ZHAO Xiangyuan, HU Xiangyang, et al. Development characteristics and distribution patterns of natural fractures of continental reservoir in Yuanba area, northeastern Sichuan Basin[J]. Fault-Block Oil and Gas Field, 2022, 29(1): 8-13. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT202201002.htm [37] 赵文智, 胡素云, 汪泽成, 等. 鄂尔多斯盆地基底断裂在上三叠统延长组石油聚集中的控制作用[J]. 石油勘探与开发, 2003, 30(5): 1-5. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200305000.htmZHAO Wenzhi, HU Suyun, WANG Zecheng, et al. Key role of basement fault control on oil accumulation of Yanchang Formation, Upper Triassic, Ordos Basin[J]. Petroleum Exploration and Development, 2003, 30(5): 1-5. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200305000.htm [38] 吴忠锐, 何生, 何希鹏, 等. 涟源凹陷上二叠统大隆组泥页岩裂缝方解石脉体流体包裹体特征及其启示[J]. 地质科技情报, 2019, 38(4): 70-81. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201904009.htmWU Zhongrui, HE Sheng, HE Xipeng, et al. Characteristics of fluid inclusions in fracture calcite veins and implications of Upper Permain Dalong Formation shale at the Lianyuan Depression[J]. Geological Science and Technology Information, 2019, 38(4): 70-81. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201904009.htm [39] 何自新. 鄂尔多斯盆地演化与油气[M]. 北京: 石油工业出版社, 2003.HE Zixin. The evolution and petroleum of Ordos Basin[M]. Beijing: Petroleum Industry Press, 2003. [40] 祖克威, 曾联波, 巩磊. 断层相关褶皱概念模型中的裂缝域[J]. 地质科学, 2013, 48(4): 1140-1147. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX201304012.htmZU Kewei, ZENG Lianbo, GONG Lei. Fractures domains in conceptual models of fault-related folds[J]. Chinese Journal of Geology, 2013, 48(4): 1140-1147. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX201304012.htm [41] 刘永涛, 刘池洋, 赵俊峰, 等. 鄂尔多斯盆地西缘中部微小断层的成因机制与控藏特征[J]. 地质科学, 2018, 53(3): 922-940.LIU Yongtao, LIU Chiyang, ZHAO Junfeng, et al. Forming mechanism of small-scale faults and their control for the reservoir formation in the middle of western margin of the Ordos Basin[J]. Chinese Journal of Geology, 2018, 53(3): 922-940. [42] 徐黎明, 周立发, 张义楷, 等. 鄂尔多斯盆地构造应力场特征及其构造背景[J]. 大地构造与成矿学, 2006, 30(4): 455-462. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK200604006.htmXU Liming, ZHOU Lifa, ZHANG Yikai, et al. Characteristics and tectonic setting of tectono-stress field of Ordos Basin[J]. Geotectonica et Metallogenia, 2006, 30(4): 455-462. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK200604006.htm [43] 刘亢, 曹代勇, 徐浩, 等. 鄂尔多斯煤盆地西缘古构造应力场演化分析[J]. 中国煤炭地质, 2014, 26(8): 87-90. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGMT201408020.htmLIU Kang, CAO Daiyong, XU Hao, et al. Paleotectonic stress field evolutional analysis in west margin of Ordos coal basin[J]. Coal Geology of China, 2014, 26(8): 87-90. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGMT201408020.htm [44] 赵红格, 刘池洋, 王建强, 等. 鄂尔多斯盆地西部晚三叠世构造属性探讨[J]. 中国地质, 2007, 34(3): 384-391. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200703005.htmZHAO Hongge, LIU Chiyang, WANG Jianqiang, et al. Tectonic attribute of the western Ordos Basin during the Late Triassic[J]. Geology in China, 2007, 34(3): 384-391. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200703005.htm [45] 周新平, 惠潇, 邓秀芹, 等. 鄂尔多斯盆地盐池地区中生界油藏分布规律及成藏主控因素[J]. 西北大学学报(自然科学版), 2019, 49(2): 268-279. https://www.cnki.com.cn/Article/CJFDTOTAL-XBDZ201902015.htmZHOU Xinping, HUI Xiao, DENG Xiuqin, et al. Distribution and main controlling factors of Mesozoic reservoir in Yanchi area of Ordos Basin[J]. Journal of Northwest University (Natural Science Edition), 2019, 49(2): 268-279. https://www.cnki.com.cn/Article/CJFDTOTAL-XBDZ201902015.htm [46] 屈雪峰, 温德顺, 张龙, 等. 鄂尔多斯盆地延长组超低渗透油藏形成过程分析: 以古峰庄—麻黄山地区为例[J]. 沉积学报, 2017, 35(2): 383-392. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201702015.htmQU Xuefeng, WEN Deshun, ZHANG Long, et al. Accumulation process of ultra-low permeability reservoirs in Yanchang Formation Ordos Basin: a case from Gufengzhuang-Mahuangshan area[J]. Acta Sedimentologica Sinica, 2017, 35(2): 383-392. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201702015.htm -
点击查看大图
图(10) / 表(1)
计量
- 文章访问数: 429
- HTML全文浏览量: 148
- PDF下载量: 61
- 被引次数: 0
苏公网安备32021102000780号