Hydrocarbon charging stage and accumulation mode of forward fault step zone in fault basin: taking the Chengbei fault step zone in Qikou Sag, Bohai Bay Basin as an example
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摘要: 我国东部断陷湖盆多发育断阶带构造，其中顺向断阶带比例较高，其时空配置关系和油气成藏期次、成藏条件对区域油气勘探地质评价起着关键性作用，但研究难度大。渤海湾盆地歧口凹陷埕北断阶带是具有典型意义的顺向断阶带，为了进一步明确其油气成藏模式和充注期次，以古近系东营组和沙河街组为主要目的层，选取歧东3-1井、张10井和埕海16井分别代表断阶区的低、中、高断阶，通过储层显微岩相观察、流体包裹体鉴定、盐水包裹体均一温度和盐度测试、GOI统计分析等技术，对埕北各区不同充注期的油气性质和分布规律进行了研究；应用激光拉曼测试对张10井和歧东3-1井单个包裹体的气体成分进行有效识别，结合歧东3-1井单井埋藏史、古地温史图和自生伊利石K-Ar同位素测年技术，确定出埕北断阶区的具体油气成藏时间，并在调研和样品实验的基础上总结了埕北区的烃源岩、储集层、保存和运聚4个成藏要素条件。研究区储层存在2期充注：第一期油气具体成藏时间在东营末期—馆陶初期, 约16 Ma左右；第二期成藏时间在明化镇初期, 从6 Ma左右开始延续至今。研究区具有多套生储盖层，发育的断阶构造对源储的沟通和油气的封堵、保存和运聚成藏起到控制作用；区域成藏条件较为成熟，在油气成藏过程中体现出双源供烃、多期成藏的横向运聚模式和断砂耦合、接力爬坡的纵向运聚模式。Abstract: Fault step zones are well developed in faulted lake basins in the eastern part of China, among which, forward fault step zones account for a large proportion, and their spatiotemporal configuration relationship, oil and gas accumulation periods and accumulation conditions, which play a key role in the geological evaluation of regional oil and gas exploration, are difficult to study. In order to further clarify its hydrocarbon accumulation mode and filling period, the authors, by taking the Paleogene Dongying and Shahejie formations in the study area as the main target layers, and selecting wells Qidong 3-1, Zhang 10 and Chenghai 16 to represent the low, medium and high fault levels of the fault area, respectively, conducted in-depth research on the oil and gas properties and distribution laws of different charging stages in various districts of Chengbei through reservoir microlithography observation, fluid inclusion identification, salt water inclusion homogenization temperature and salinity test, GOI statistical analysis and other technologies; applied laser Raman test to effectively identify the gas composition of single inclusions in wells Zhang-10 and Qidong 3-1, determined the specific oil and gas accumulation time in Chengbei fault step zone in combination with the single well burial history, paleogeothermal history and autoclastic illite K-Ar isotopic dating technology of well Qidong 3-1, and summarized the four accumulation elements of source rocks, reservoirs, preservation and transportation in Chengbei area. There are two charging stages in the reservoir, the specific accumulation time of the first stage is from the end of Dongying to the early stage of Guantao, about 16 Ma ±, while that of the second stage is in the early stage of Minghua Town, starting from 6 Ma ± and continuing to the present. Multiple sets of reservoir layers are developed in the study area, and the special fault step structure plays a controlling role in channeling the source rocks and reservoirs, the sealing and preservation of oil and gas, and the transportation and accumulation of reservoirs. The regional accumulation conditions are relatively mature, and the lateral migration-accumulation mode of dual-source hydrocarbon supply and multi-stage accumulation and the longitudinal migration-accumulation mode of fault-sand coupling and relay climbing are reflected in the process of oil and gas accumulation.
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图 1 渤海湾盆地歧口凹陷埕北断阶带构造位置及地层综合柱状图
Figure 1. Comprehensive histogram of structural location and stratigraphy of Chengbei fault step zone in Qikou Sag, Bohai Bay Basin
图 2 渤海湾盆地歧口凹陷埕北断阶带储层典型包裹体显微照片
据大港油田资料修改。
a.歧东3-1井，东营组，2 576 m, 石英颗粒次生加大，局部孔隙充填沥青，发育弱绿色荧光包裹体，荧光；b.歧东3-1井，东营组，2 576 m, 发育浅黄色荧光气液烃包裹体，荧光；c.歧东3-1井，沙一段，3 791 m, 孔隙中轻质油显示黄绿色荧光，荧光；d.歧东3-1井，沙一段，3 686 m, 砂岩微裂缝和粒间孔隙充填深褐色沥青，单偏光；e.歧东3-1井，沙二段，3 935~3 965 m，微裂缝发育，单偏光；f.歧东3-1井，沙二段，3 935~3 965 m，蓝绿色气液烃包裹体沿微裂缝成带分布，荧光；g.张10井，沙二段，3 305 m, 轻质油显示强绿色荧光，荧光；h.张10井，沙二段，3 302.6 m, 轻质油显示黄绿色荧光，荧光；i.张10井，沙三段，3 420 m，晚期亮晶方解石胶结物，单偏光；j.张10井，沙三段，3 420 m，发育黄绿色荧光气液烃包裹体，为i对应的荧光照片；k.埕海16井，沙一段，1 335 m, 砂岩粒间孔隙中充填深褐色稠油沥青，单偏光；l.埕海16井，沙一段，1 335 m，沿石英愈合裂隙分布深褐色液烃包裹体，单偏光。Figure 2. Micrographs of typical inclusions in reservoirs of Chengbei fault step zone in Qikou Sag, Bohai Bay Basin
图 3 渤海湾盆地歧口凹陷埕北断阶带典型井包裹体均一温度(a)、盐度分布(b)
Figure 3. Homogenization temperature (a) and salinity (b) distributions of inclusions in typical wells in Chengbei fault step zone, Qikou Sag, Bohai Bay Basin
图 4 渤海湾盆地歧口凹陷埕北断阶带流体包裹体激光拉曼谱图
Figure 4. Laser Raman spectrograms of fluid inclusions in Chengbei fault step zone, Qikou Sag, Bohai Bay Basin
图 5 渤海湾盆地歧口凹陷埕北断阶带油气成藏时间综合图(歧东3-1井)
Figure 5. Comprehensive diagram of hydrocarbon accumulation time in Chengbei fault step zone, Qikou Sag, Bohai Bay Basin (well Qidong 3-1)
图 6 渤海湾盆地歧口凹陷埕北断阶带沙河街组烃源岩有机地球化学特征
Figure 6. Organic geochemical characteristics of Shahejie Formation source rocks in Chengbei fault step zone, Qikou Sag, Bohai Bay Basin
图 7 渤海湾盆地歧口凹陷埕北断阶区各层位储层物性直方图
Figure 7. Histogram of reservoir properties at each zone in Chengbei fault step zone, Qikou Sag, Bohai Bay Basin
图 8 渤海湾盆地歧口凹陷埕北断阶带油气横向运聚成藏
Figure 8. Lateral migration and accumulation of oil and gas in Chengbei fault step zone, Qikou Sag, Bohai Bay Basin
图 9 渤海湾盆地歧口凹陷埕北断阶带油气垂向运聚成藏
据大港油田资料修改。
Figure 9. Vertical migration and accumulation of oil and gas in Chengbei fault step zone, Qikou Sag, Bohai Bay Basin
表 1 渤海湾盆地歧口凹陷埕北断阶带储层孔隙荧光与GOI特征统计
Table 1. Statistics of pore fluorescence and GOI characteristics of reservoirs in Chengbei fault step zone in Qikou Sag, Bohai Bay Basin
断阶位置 井号 层位 深度/m 荧光特性 GOI统计 含油性 低断阶 歧东3-1井 Ed 2 576 局部粒间孔隙中含中轻质油，显示绿色荧光；砂岩局部粒间孔隙中还充填有灰黑色、无荧光显示、反映早期少量油气充注的固体沥青 早期1%；晚期≤0.5% 水层 Es1 3 686 粒间孔隙不含油，无荧光显示；局部微裂缝中充填有深褐色、无荧光显示、反映早期少量油气充注的稠油沥青 早期1% 不含油 Es1 3 791 粒间孔隙中含中轻质油，普遍显示黄绿色荧光 早期1%；晚期35% 差油层 Es2 3 935~3 965 部分粒屑粒间孔隙中充填有灰黑色、无荧光显示、反映早期少量油气充注的固体沥青 早期1%；晚期≤0.5% 干层 中断阶 张10井 Es2 3 302 部分粒间孔隙中含中轻质油，显示黄绿色荧光；局部粒间孔隙中充填有灰黑色、无荧光显示、反映早期少量油气充注的固体沥青 早期8%；晚期5% 含油层 Es2 3 305 粒间孔隙中饱含中轻质油，显示绿黄色荧光；部分粒间孔隙中充填有灰黑色、无荧光显示、反映早期少量油气充注的固体沥青 早期4%；晚期3% 油层 Es3 3 420 部分粒间孔隙中饱含中轻质油，显示黄绿色荧光；局部粒间孔隙中还充填有黑褐色、无荧光显示、反映早期少量油气充注的固体沥青 早期6%；晚期5% 油层 高断阶 埕海16井 Es1 1 335 粒间孔隙中普遍充填有深褐色、无荧光显示、反映早期大量油气充注的稠油沥青 早期1%；晚期3% 油层 
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表 2 包裹体组分对应的特征拉曼谱峰
Table 2. Characteristic Raman peaks corresponding to inclusion components
成分 拉曼峰值/cm-1 成分 拉曼峰值/cm-1 N2 2 328~2 333 CO2 1 386~1 390 CO 2 143~2 146 H2S 2 609~2 613 H2O 3 645~3 750 CH4 2 909~2 915
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表 3 渤海湾盆地歧口凹陷沙河街组储层自生伊利石K-Ar年龄
Table 3. K-Ar isotopic dating of autoclastic illites in Shahejie Formation reservoirs, Qikou Sag, Bohai Bay Basin
井号 层位 井深/m K-Ar年龄/Ma 歧东3-1井 Es1 3 791 15~23 Es2 3 945 22~32 Es3 4 250 25~32
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[1] 曲江秀, 查明, 高长海, 等. 大港油田埕北断阶带油气运移、成藏期次及成藏模式[J]. 海相油气地质, 2009, 14(3): 37-45. https://www.cnki.com.cn/Article/CJFDTOTAL-HXYQ200903009.htmQU Jiangxiu, ZHA Ming, GAO Changhai, et al. Models of hydrocarbon migration and accumulation in Chengbei fault-step belt in Dagang oil field[J]. Marine Origin Petroleum Geology, 2009, 14(3): 37-45. https://www.cnki.com.cn/Article/CJFDTOTAL-HXYQ200903009.htm [2] 袁淑琴, 丁新林, 苏俊青, 等. 大港油田滩海区埕北断阶带油气成藏条件研究[J]. 江汉石油学院学报, 2004, 26(S1): 8-9. https://www.cnki.com.cn/Article/CJFDTOTAL-JHSX2004S1003.htmYUAN Shuqin, DING Xinlin, SU Junqing, et al. Study on oil and gas accumulation conditions in Chengbei fault zone in the beach sea area of Dagang Oilfield[J]. Journal of Jianghan Petroleum Institute, 2004, 26(S1): 8-9. https://www.cnki.com.cn/Article/CJFDTOTAL-JHSX2004S1003.htm [3] 张育民. 塔里木盆地卡塔克隆起斜坡区油气成藏期次研究[J]. 石油实验地质, 2021, 43(6): 1015-1023. doi: 10.11781/sysydz2021061015ZHANG Yumin. Petroleum charge history of the slope area of Katake Uplift in Tarim Basin[J]. Petroleum Geology & Experiment, 2021, 43(6): 1015-1023. doi: 10.11781/sysydz2021061015 [4] 刘世豪, 林小云, 刘建. 济源凹陷中生界流体包裹体特征与油气成藏期次[J]. 海洋地质前沿, 2020, 36(4): 55-60. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDT202004006.htmLIU Shihao, LIN Xiaoyun, LIU Jian. Characteristics of fluid inclusions and hydrocarbon accumulation phases of the Mesozoic in the Jiyuan Sag[J]. Marine Geology Frontiers, 2020, 36(4): 55-60. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDT202004006.htm [5] CUI Jingwei, ZHANG Zhongyi, ZHANG Yan, et al. Oil and gas accumulation periods and charging path of continental lake basin: a case study of the Chang 9-Chang 10 oil reservoir in the Yanchang Formation in the Ordos Basin[J]. Journal of Petroleum Science and Engineering, 2022, 219: 111136. doi: 10.1016/j.petrol.2022.111136 [6] LUBOńK, TARKOWSKI R. The influence of the first filling period length and reservoir level depth on the operation of underground hydrogen storage in a deep aquifer[J]. International Journal of Hydrogen Energy, 2023, 48(3): 1024-1042. doi: 10.1016/j.ijhydene.2022.09.284 [7] LOU Renxing, WANG Liwu, WANG Lixian, et al. Characteristics of fluid inclusions and hydrocarbon accumulation period of Huoshiling-Yingcheng formations in Wangfu Fault Depression, Songliao Basin, China[J]. Journal of Petroleum Science and Engineering, 2022, 208: 109421. doi: 10.1016/j.petrol.2021.109421 [8] 刘文超, 叶加仁, 郭飞飞. 油气成藏期研究方法[J]. 海洋地质前沿, 2011, 27(8): 59-65. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDT201108010.htmLIU Wenchao, YE Jiaren, GUO Feifei. A review of the methods for determination of hydrocarbon reservoir forming stages[J]. Marine Geology Frontiers, 2011, 27(8): 59-65. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDT201108010.htm [9] 张洪, 赵贤正, 王居峰, 等. 歧口凹陷埕北断阶带油气输导体系及其控藏作用[J/OL]. 地球科学: 1-15[2022-11-03]. http://kns.cnki.net/kcms/detail/42.1874.P.20220218.1154.004.html .ZHANG Hong, ZHAO Xianzheng, WANG Jufeng, et al. Oil and gas transmission system and its reservoir control effect in the northern fault zone of Qikou Sag Depression[J/OL]. Earth Science: 1-15[2022-11-03].http://kns.cnki.net/kcms/detail/42.1874.P.20220218.1154.004.html .[10] 缪欢, 王延斌, 何川, 等. 渤海湾盆地埕北断阶带断裂发育特征及其控藏作用[J]. 岩性油气藏, 2022, 34(2): 105-115. https://www.cnki.com.cn/Article/CJFDTOTAL-YANX202202010.htmMIAO Huan, WANG Yanbin, HE Chuan, et al. Fault development characteristics and reservoir control in Chengbei fault step zone, Bohai Bay Basin[J]. Lithologic Reservoirs, 2022, 34(2): 105-115. https://www.cnki.com.cn/Article/CJFDTOTAL-YANX202202010.htm [11] 文杰. 歧口凹陷埕北断阶带油气运聚成藏机制研究[D]. 青岛: 中国石油大学, 2010.WEN Jie. Research on mechanism of the hydrocarbon migration and accumulation in Chengbei step-fault zone, Qikou Depression[D]. Qingdao: China University of Petroleum, 2010. [12] 许浚远, 张凌云, 杨东胜, 等. 歧口凹陷构造演化[J]. 石油实验地质, 1996, 18(4): 348-355. doi: 10.11781/sysydz199604348XU Junyuan, ZHANG Lingyun, YANG Dongsheng, et al. Tectonic evolution of Qikou Depression in the Bohaiwan Basin of East China[J]. Experimental Petroleum Geology, 1996, 18(4): 348-355. doi: 10.11781/sysydz199604348 [13] 韩国猛, 司维柳, 石倩茹, 等. 歧北斜坡岩性油气藏成藏条件与有利区带优选[J]. 天然气地球科学, 2010, 21(4): 594-600. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX201004013.htmHAN Guomeng, SI Weiliu, SHI Qianru, et al. Conditions of lithologic reservoir formation and favorable selection of exploration area in north slope of Qikou Sag[J]. Natural Gas Geoscience, 2010, 21(4): 594-600. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX201004013.htm [14] 袁淑琴, 于长华, 董晓伟, 等. 歧口凹陷埕海断坡区古近系油气成藏条件与富集因素分析[J]. 新疆地质, 2011, 29(1): 71-74. https://www.cnki.com.cn/Article/CJFDTOTAL-XJDI201101016.htmYUAN Shuqin, YU Changhua, DONG Xiaowei, et al. Analysis on the hydrocarbon accumulation conditions and main controlling factors of Paleogene in Chenghai fult-slope, Qikou Depression[J]. Xinjiang Geology, 2011, 29(1): 71-74. https://www.cnki.com.cn/Article/CJFDTOTAL-XJDI201101016.htm [15] 张杰, 邱楠生, 韦阿娟, 等. 黄骅坳陷歧口凹陷隐蔽油气藏形成条件与分布规律[J]. 西安石油大学学报(自然科学版), 2005, 20(3): 32-35. https://www.cnki.com.cn/Article/CJFDTOTAL-XASY200503007.htmZHANG Jie, QIU Nansheng, WEI Ajuan, et al. Discussion on the accumulation conditions and the distribution of the subtle traps in Qikou Sag, Huanghua Depression[J]. Journal of Xi'an Shiyou University (Natural Science Edition), 2005, 20(3): 32-35. https://www.cnki.com.cn/Article/CJFDTOTAL-XASY200503007.htm [16] 王秀红, 陈涛, 李政, 等. 济阳坳陷滩海地区埕北斜394井凝析油气特征及形成机制[J]. 油气地质与采收率, 2021, 28(3): 35-41. https://www.cnki.com.cn/Article/CJFDTOTAL-YQCS202103005.htmWANG Xiuhong, CHEN Tao, LI Zheng, et al. Characteristics and formation mechanism of condensate oil and gas from Well CBX394 in Jiyang Depression[J]. Petroleum Geology and Recovery Efficiency, 2021, 28(3): 35-41. https://www.cnki.com.cn/Article/CJFDTOTAL-YQCS202103005.htm [17] 刘德汉. 包裹体研究——盆地流体追踪的有力工具[J]. 地学前缘, 1995, 2(3/4): 149-154. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY504.002.htmLIU Dehan. Fluid inclusion studies: an effective means for basin fluid investigation[J]. Earth Science Frontiers, 1995, 2(3/4): 149-154. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY504.002.htm [18] 林红梅, 程付启, 王永诗, 等. 渤海湾盆地渤南洼陷沙四段油气多期充注的流体包裹体证据[J]. 石油与天然气地质, 2017, 38(2): 209-218. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201702002.htmLIN Hongmei, CHENG Fuqi, WANG Yongshi, et al. Fluid inclusion evidence for multi-period oil charge in Shahejie member 4, Bonan Subsag, Bohai Bay Basin[J]. Oil & Gas Geology, 2017, 38(2): 209-218. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201702002.htm [19] 池国祥, 周义明, 卢焕章. 当前流体包裹体研究和应用概况(英文)[J]. 岩石学报, 2003, 19(2): 201-212. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200302000.htmCHI Guoxiang, ZHOU Yiming, LU Huanzhang. An overview on current fluid-inclusion research and applications[J]. Acta Petrologica Sinica, 2003, 19(2): 201-212. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200302000.htm [20] 赵靖舟. 油气包裹体在成藏年代学研究中的应用实例分析[J]. 地质地球化学, 2002, 30(2): 83-89. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDQ200202014.htmZHAO Jingzhou. Hydrocarbon inclusion analysis: application in geochronological study of hydrocarbon accumulation[J]. Geology-Geochemistry, 2002, 30(2): 83-89. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDQ200202014.htm [21] 夏茂龙, 范毅, 江蓉蓉, 等. 四川盆地东北部飞仙关组储层流体包裹体特征[J]. 石油学报, 2012, 33(S2): 74-81. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB2012S2006.htmXIA Maolong, FAN Yi, JIANG Rongrong, et al. The characteristics of fluid inclusions in Feixianguan Formation, northeastern Sichuan Basin, China[J]. Acta Petrolei Sinica, 2012, 33(S2): 74-81. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB2012S2006.htm [22] 成科璋, 崔军平, 孟张勇, 等. 鄂尔多斯盆地吴起地区延安组储层流体包裹体特征与油气成藏期次分析[J/OL]. 中国地质: 1-19[2023-05-06]. http://kns.cnki.net/kcms/detail/11.1167.P.20220418.1459.006.html .CHENG Kezhang, CUI Junping, MENG Zhangyong, et al. Characte-ristics of reservoir fluid inclusions and oil and gas accumulation period analysis in Yan'an Formation in Wuqi area, Ordos Basin[J/OL]. Geology in China: 1-19[2023-05-06].http://kns.cnki.net/kcms/detail/11.1167.P.20220418.1459.006.html .[23] 徐良, 杨光, 夏淑华. 流体包裹体技术在油气成藏期次研究中的应用: 以黑帝庙地区为例[J]. 吉林大学学报(地球科学版), 2006, 36(S1): 29-32. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ2006S1006.htmXU Liang, YANG Guang, XIA Shuhua. Applitation of fluid inclusions in study of the times and stages of hydrocarbon reservior filling: a case study of Heidimiao area in south Songliao Basin[J]. Journal of Jilin University (Earth Science Edition), 2006, 36(S1): 29-32. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ2006S1006.htm [24] 税蕾蕾, 郭来源, 徐新德, 等. 莺歌海盆地乐东10区CO2包裹体特征及其流体充注史[J]. 石油实验地质, 2021, 43(5): 835-843. doi: 10.11781/sysydz202105835SHUI Leilei, GUO Laiyuan, XU Xinde, et al. Fluid charging history in Ledong 10 area, Yinggehai Basin, revealed by CO2 inclusion characteristics[J]. Petroleum Geology & Experiment, 2021, 43(5): 835-843. doi: 10.11781/sysydz202105835 [25] 席斌斌, 蒋宏, 许锦, 等. 基于包裹体PVTx数值模拟恢复油藏古温压: 存在的问题、对策及应用实例[J]. 石油实验地质, 2021, 43(5): 886-895. doi: 10.11781/sysydz202105886XI Binbin, JIANG Hong, XU Jin, et al. Reconstruction of paleo-temperature and pressure of oil reservoirs based on PVTx simulation: problems, strategies and case studies[J]. Petroleum Geo-logy & Experiment, 2021, 43(5): 886-895. doi: 10.11781/sysydz202105886 [26] 何谋春, 吕新彪, 王群英. 有机包裹体的拉曼光谱测定[J]. 石油实验地质, 2002, 24(2): 181-183. doi: 10.11781/sysydz200202181HE Mouchun, LÜ Xinbiao, WANG Qunying. Measurement of laser Raman spectra in organic fluid inclusions[J]. Petroleum Geology & Experiment, 2002, 24(2): 181-183. doi: 10.11781/sysydz200202181 [27] 胡凯, 刘英俊, WILLEINS R W T. 沉积有机质的喇曼光谱研究[J]. 沉积学报, 1993, 11(3): 64-71. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB199303009.htmHU Kai, LIU Yingjun, WILLEINS R W T. Raman spectral studies of sedimentary organic matter[J]. Acta Sedimentologica Sinica, 1993, 11(3): 64-71. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB199303009.htm [28] 刘小平, 邱楠生. 黄骅坳陷歧口凹隐蔽油气藏成藏期分析[J]. 石油天然气学报(江汉石油学院学报), 2006, 28(3): 203-205. https://www.cnki.com.cn/Article/CJFDTOTAL-JHSX200603064.htmLIU Xiaoping, QIU Nansheng. Analysis of reservoir formation period of hidden oil and gas reservoirs in Huanghua Depression[J]. Journal of Oil and Gas Technology (Journal of Jianghan Petroleum Institute), 2006, 28(3): 203-205. https://www.cnki.com.cn/Article/CJFDTOTAL-JHSX200603064.htm [29] 任战利, 刘丽, 崔军平, 等. 盆地构造热演化史在油气成藏期次研究中的应用[J]. 石油与天然气地质, 2008, 29(4): 502-506. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT200804016.htmREN Zhanli, LIU Li, CUI Junping, et al. Application of tectonic-thermal evolution history to hydrocarbon accumulation timing in sedimentary basins[J]. Oil & Gas Geology, 2008, 29(4): 502-506. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT200804016.htm [30] 蒋有录, 苏圣民, 刘华等. 渤海湾盆地油气成藏期差异性及其主控因素[J]. 石油与天然气地质, 2021, 42(6): 1255-1264. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT202106002.htmJIANG Youlu, SU Shengmin, LIU Hua, et al. Differences in hydrocarbon accumulation stages and main controlling factors in the Bohai Bay Basin[J]. Oil & Gas Geology, 2021, 42(6): 1255-1264. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT202106002.htm [31] 张芷晴, 刘华, 马立驰, 等. 渤海湾盆地济阳坳陷潜山油气藏成藏期次和过程: 来自储层流体包裹体的证据[J]. 石油实验地质, 2022, 44(1): 129-138. doi: 10.11781/sysydz202201129ZHANG Zhiqing, LIU Hua, MA Lichi, et al. Characteristics of reservoir fluid inclusions and hydrocarbon charging process in the Dawangzhuang buried hill zone of Jiyang Depression, Bohai Bay Basin[J]. Petroleum Geology & Experiment, , 2022, 44(1): 129-138. doi: 10.11781/sysydz202201129 [32] 张有瑜, ZWINGMANN H, 刘可禹, 等. 自生伊利石K-Ar、Ar-Ar测年技术对比与应用前景展望: 以苏里格气田为例[J]. 石油学报, 2014, 35(3): 407-416. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB201403003.htmZHANG Youyu, ZWINGMANN H, LIU Keyu, et al. Perspective on the K/Ar and Ar/Ar geochronology of authigenic illites: a case study from the Sulige gas field, Ordos Basin, China[J]. Acta Petrolei Sinica, 2014, 35(3): 407-416. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB201403003.htm [33] 张有瑜, 罗修泉. 油气储层自生伊利石分离提纯微孔滤膜真空抽滤装置与技术[J]. 石油实验地质, 2011, 33(6): 671-676. doi: 10.11781/sysydz201106671ZHANG Youyu, LUO Xiuquan. A vacuum filtrating device and technique to separate authigenic illites from sandstone reservoirs with microporous membrane[J]. Petroleum Geology & Experiment, 2011, 33(6): 671-676. doi: 10.11781/sysydz201106671 [34] 张有瑜, 罗修泉, 宋健. 油气储层中自生伊利石K-Ar同位素年代学研究若干问题的初步探讨[J]. 现代地质, 2002, 16(4): 403-407. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ200204010.htmZHANG Youyu, LUO Xiuquan, SONG Jian. Discussions on K-Ar isotopic geochronological studies of authigenic illites in hydrocarbon reservoirs[J]. Geoscience, 2002, 16(4): 403-407. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ200204010.htm [35] 李会军, 吴泰然, 马宗晋, 等. 黄骅坳陷古近系深层烃源岩成烃演化特征[J]. 石油勘探与开发, 2004, 31(6): 40-43. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200406010.htmLI Huijun, WU Tairan, MA Zongjin, et al. Hydrocarbon generation from Paleogene deep source rocks in Huanghua Depression[J]. Petroleum Exploration and Development, 2004, 31(6): 40-43. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200406010.htm [36] 吴元燕, 付建林, 周建生, 等. 歧口凹陷含油气系统及其评价[J]. 石油学报, 2000, 21(6): 18-22. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB200006004.htmWU Yuanyan, FU Jianlin, ZHOU Jiansheng, et al. Evaluation of hydrocarbon system in Qikou Sag[J]. Acta Petrolei Sinica, 2000, 21(6): 18-22. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB200006004.htm [37] 王振升, 于学敏, 国建英, 等. 歧口凹陷天然气地球化学特征及成因分析[J]. 天然气地球科学, 2010, 21(4): 683-691. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX201004030.htmWANG Zhensheng, YU Xuemin, GUO Jianying, et al. Geochemical characteristics and genesis of natural gas in Qikou Sag[J]. Natural Gas Geoscience, 2010, 21(4): 683-691. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX201004030.htm [38] 杨有星, 金振奎. 黄骅坳陷港中地区古近系沙三段湖底扇沉积相特征[J]. 现代地质, 2012, 26(2): 355-362. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ201202018.htmYANG Youxing, JIN Zhenkui. Sedimentary characteristics of sublacustrine fan of the third member of Shahejie Formation in Gangzhong Oilfield, Huanghua Depression[J]. Geoscience, 2012, 26(2): 355-362. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ201202018.htm [39] 杨国安, 邢卫东, 刘广华, 等. 港中开发区沙河街组沉积微相与油气分布[J]. 西北大学学报(自然科学版), 2004, 34(1): 93-96. https://www.cnki.com.cn/Article/CJFDTOTAL-XBDZ200401025.htmYANG Guoan, XING Weidong, LIU Guanghua, et al. The lacustrine reservoir microface models and gas-oil distribution in Shahejie Formation of Gangzhong Oilfield[J]. Journal of Northwest University (Natural Science Edition), 2004, 34(1): 93-96. https://www.cnki.com.cn/Article/CJFDTOTAL-XBDZ200401025.htm [40] 朱娜娜. 歧口凹陷沙河街组一段中部泥岩盖层封闭性综合评价[D]. 大庆: 东北石油大学, 2012.ZHU Nana. Comprehensive evaluation of mudstone caprocks in the middle of the first member of Shahejie Fm in the Qikou Sag[D]. Daqing: Northeast Petroleum University, 2012. [41] 史集建, 付广, 吕延防, 等. 歧口凹陷沙河街组一段中部区域盖层封气能力综合评价[J]. 石油与天然气地质, 2011, 32(5): 671-681. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201105009.htmSHI Jijian, FU Guang, LÜ Yanfang, et al. Comprehensive evaluation of regional seal in the middle of the first member of Shahejie Fm in the Qikou Sag[J]. Oil & Gas Geology, 2011, 32(5): 671-681. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201105009.htm [42] 杨晓敏, 罗群, 黄捍东, 等. 顺向断坡油气藏分布特征及成藏主控因素: 以孤北斜坡为例[J]. 油气地质与采收率, 2008, 15(1): 10-13. https://www.cnki.com.cn/Article/CJFDTOTAL-YQCS200801004.htmYANG Xiaomin, LUO Qun, HUANG Handong, et al. Distribution and main controlling factors of hydrocarbon reservoirs in consequent fault-slope: a case study of Gubei Slope[J]. Petroleum Geology and Recovery Efficiency, 2008, 15(1): 10-13. https://www.cnki.com.cn/Article/CJFDTOTAL-YQCS200801004.htm [43] 吴安彬, 罗群, 崔倩, 等. 断陷盆地顺向断坡油气优势运移通道及聚油模式: 以渤海湾盆地沾化凹陷孤北斜坡为例[J]. 东北石油大学学报, 2020, 44(1): 53-64. https://www.cnki.com.cn/Article/CJFDTOTAL-DQSY202001007.htmWU Anbin, LUO Qun, CUI Qian, et al. Dominant migration pathway and accumulation model of petroleum along the consequent fault slope in the fault basin: taking Gubei Slope of Zhanhua Sag in the Bohai Bay Basin as an example[J]. Journal of Northeast Petroleum University, 2020, 44(1): 53-64. https://www.cnki.com.cn/Article/CJFDTOTAL-DQSY202001007.htm -
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