Pathway System of Large-Scale Petroleum System and Its Controls on Hydrocarbon Accumulation in the Bozhong Sub-Basin, Bohai Bay Basin
-
摘要: 渤中坳陷东营组沉积期以来快速沉降和强烈断裂活动的地质背景导致其呈现出不同于渤海湾盆地其他地区的油气成藏特征.凹陷周缘凸起带成为油气聚集的主要场所, 输导体系的分布与演化控制了油气运移和成藏.在阐明渤中坳陷大型油气系统烃源岩和油气分布规律的基础上, 综合利用多种资料分析了各类潜在输导通道的发育特征及其空间配置, 识别出断裂主导型、砂体主导型和不整合主导型3类控藏输导体系.凸起边缘继承性的长期断层充当了垂向流体释放和油气运移的主输导通道, 控制了凸起带上新近系储集层中的油气聚集.特别是在构造活跃期, 开启的长期断层成为油气快速垂向运移的首选通道.古近系沙河街组和东营组的连通性砂体与活跃烃源岩直接接触, 不仅是早期油气运移和聚集的主要场所, 也是晚期油气运移和聚集的始发站.因此, 它们不仅控制了古近系圈闭的油气聚集, 同时在很大程度上直接控制了凸起带新近系圈闭的油气供给.不整合T8是中生代末区域构造变革的产物, 其渗透性因风化作用而得以提高, 充当了深部侧向油气运移的输导通道, 控制了潜山储集层中的油气成藏.3类输导体系对油气成藏的时间、部位、速率和规模等都具有不同程度的影响, 但断裂主导型输导体系的控制作用最为显著.Abstract: The geological evolution of the Bozhong sub-basin, characterized by rapid subsidence and strong fault activities since the initiation of the Dongying Formation, exerts important effect on the characteristics of hydrocarbon accumulation in this area, which is distinguished from those in other areas in the Bohai Bay Basin. Uplifts around depressions serve as predominant sites for hydrocarbon accumulation, and the distribution and evolution of pathway systems have obviously been controlling hydrocarbon migration and accumulation. Based on clarification of the distribution of hydrocarbon source rocks and petroleum resources in the large-scale Bozhong petroleum system, growing characteristics of all kinds of potential pathways and their spatial relevance are analyzed by means of multiple data, and then three pathway system types controlling hydrocarbon migration and accumulation: fault-dominant, carrier bed-dominant and unconformity-dominant types are identified. Long-term growth faults adjoining uplifts act as the predominant pathways for vertical fluid release and hydrocarbon migration, and control hydrocarbon accumulation in the Neogene reservoirs on uplifts. Especially in the active stage of tectonic movement, the open long-term growth faults must be preferential pathways for the rapid vertical hydrocarbon migration. The interconnected sandbodies in the Paleogene Shahejie and Dongying Formations, directly contacting with active hydrocarbon source rocks, serve as the primary sites and starting stations for the early and late hydrocarbon migration and accumulation, respectively. Therefore, they not only control hydrocarbon accumulation in the Paleogene traps, but also directly impact hydrocarbon supply to the Neogene trap on uplifts to some extent. Unconformity T8, resulted from regionally tectonic transformation in last Mesozoic, serve as pathway for deep lateral hydrocarbon migration and control hydrocarbon accumulation in the buried hill type reservoirs due to its improved permeability attributed to long-term weathering process. Three types of pathway systems all impact even control the times, locations, velocities and scales of hydrocarbon accumulation in various degrees. However, the fault-dominant type pathway system shows the most outstanding effect among them.
-
图 1 渤中坳陷区域位置、构造单元以及烃源岩和油气藏分布
油气藏分布据张功成等(2001)，Yang and Xu(2004)，Gong et al.(2010)，姜福杰和庞雄奇(2011)等资料编绘；现今Ro等值线据Zou et al.(2011)，用来表示沙河街组三段和东营组三段两套烃源岩的大致分布范围
Fig. 1. Regional location, structural units and distribution of source rocks and petroleum pools of the Bozhong sub-basin
图 2 渤中坳陷综合地层序列、构造-环境演化及生储盖组合(据Gong et al., 2010；何仕斌等，2001)
Fig. 2. Integrated stratigraphic column, tectonic and environmental evolution and source-reservoir-cap assemblages of the Bozhong sub-basin, Bohai bay basin
图 3 渤中坳陷3套烃源岩Ro演化剖面(剖面位置见图 1)
Fig. 3. Evolution of vitrinite reflectance in three source rock intervals of the Bozhong sub-basin
图 4 渤中坳陷构造-地层格架及油气运移剖面图(剖面位置见图 1)
Fig. 4. Section showing structural and stratigraphic framework and hydrocarbon migration of the Bozhong sub-basin
图 5 渤中坳陷油气成藏期区域应力场对主要活动断层输导能力及油气藏分布的影响
E型油气藏指最早在晚渐新世已发生油气聚集的油气藏，N型油气藏指最早在晚中新世出现油气聚集的油气藏，Q型油气藏指第四纪才发生油气聚集的油气藏.区域应力场据万天丰等(2004)编绘，断层系统据徐杰等(2011)编绘
Fig. 5. Effects of regional stress field on transporting capabilities of major active faults and the distribution of petroleum pools during the hydrocarbon migration and accumulation periods in the Bozhong sub-basin
图 6 渤中坳陷主要输导层骨架砂体分布
Fig. 6. Distribution of skeleton sandstone bodies of major carrier beds in the Bozhong sub-basin
图 7 渤中坳陷砂体输导层孔渗性能的垂向变化及其与化学成岩作用的关系
Fig. 7. Vertical changes of porosity-permeability of sandstone carrier beds and its relationship with chemical diagenesis in the Bozhong sub-basin
图 8 渤中坳陷大型油气系统油气成藏事件
Fig. 8. Event chart showing the major elements of the huge petroleum system and timing of petroleum generation and migration in the Bozhong sub-basin
-
[1] Aydin, A., 2000. Fractures, Faults, and Hydrocarbon Entrapment, Migration and Flow. Marine and Petroleum Geology, 17: 797-814. doi: 10.1016/S0264-8172(00)00020-9 [2] Boles, J.R., Eichhubl, P., Garven, G., et al., 2004. Evolution of Hydrocarbon Migration Pathway along Basin-Bounding Faults: Evidence from Fault Cement. AAPG Bulletin, 88(7): 947-970. doi: 10.1306/02090403040 [3] Cao, J., Zhang, Y.J., Hu, W.X., et al., 2005. The Permian Hybrid Petroleum System in the Northwest Margin of the Junggar Basin, Northwest China. Marine and Petroleum Geology, 22: 331-349. doi: 10.1016/j.marpetgeo.2005.01.005 [4] Deng, Y.H., 1999. Analysis of Petroleum Accumulation Difference of Sag and Uplift in Bohai Bay Basin. China Offshore Oil and Gas (Geology), 13(6): 401-405(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZHSD199906004.htm [5] Deng, Y.H., 2005. "Transfer Station" Model of Oil-Gas Migration Formed by Fault-Sandbody. China Petroleum Exploration, 10(6): 14-18(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KTSY200506003.htm [6] Deng, Y.H., Xu, C.G., Li, J.P., 2011. Discussion on the Forming Conditions of Bohai Oilfield. China Engineering Science, 13(5): 10-15(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GCKX201105004.htm [7] Galeazzi, J.S., 1998. Structural and Stratigraphic Evolution of the Western Malvinas Basin, Argentina. AAPG Bulletin, 82(4): 596-636. http://aapgbull.geoscienceworld.org/content/82/4/596 [8] Gong, Z.S., Wang, G.C., 2001. Neotectonism and Late Hydrocarbon Accumulation in Bohai Sea. Acta Petrolei Sinica, 22(2): 1-7(in Chinese with English abstract). [9] Gong, Z.S., Wang, G.C., He, Q., 2000. The Neogene: A Main Realm of Hydrocarbon Exploration in Bozhong Sag and Its Surrounding Areas. China Offshore Oil and Gas (Geology), 14(3): 145-156(in Chinese with English abstract). http://www.researchgate.net/publication/311254029_The_Neogenea_main_realm_of_hydrocarbon_exploration_in_Bozhong_sag_and_its_surrounding_areas [10] Gong, Z.S., Zhu, W.L., Chen, P.P., 2010. Revitalization of a Mature Oil-bearing Basin by a Paradigm Shift in the Exploration Concept: A Case History of Bohai Bay, Offshore China. Marine and Petroleum Geology, 27: 1011-1027. doi: 10.1016/j.marpetgeo.2009.11.010 [11] Gouze, P., Coudrain-Ribstein, A., 2002. Chemical Reactions and Porosity Changes during Sedimentary Diagenesis. Applied Geochemistry, 17: 39-47. doi: 10.1016/S0883-2927(01)00083-X [12] Hao, F., Cai, D.S., Zou, H.Y., et al., 2004. Overpressure-Tectonic Activity Controlled Fluid Flow and Rapid Petroleum Accumulation in Bozhong Depression, Bohai Bay Basin. Earth Science—Journal of China University of Geosciences, 29(5): 518-524(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200405002.htm [13] Hao, F., Zhou, X.H., Zhu, Y.M., et al., 2009. Mechanisms of Petroleum Accumulation in the Bozhong Sub-Basin, Bohai Bay Basin, China. Part 1: Origin and Occurrence of Crude Oils. Marine and Petroleum Geology, 26: 1528-1542. doi: 10.1016/j.marpetgeo.2008.09.005 [14] Hao, F., Zhou, X.H., Zhu, Y.M., et al., 2010. Charging of Oil Fields Surrounding the Shaleitian Uplift from Multiple Source Rock Intervals and Generative Kitchens, Bohai Bay Basin, China. Marine and Petroleum Geology, 27: 1910-1926. doi: 10.1016/j.marpetgeo.2010.07.005 [15] Hao, F., Zhou, X.H., Zhu, Y.M., et al., 2011. Lacustrine Source Rock Deposition in Response to Co-Evolution of Environments and Organisms Controlled by Tectonic Subsidence and Climate, Bohai Bay Basin, China. Organic Geochemistry, 42: 323-339. doi: 10.1016/j.orggeochem.2011.01.010 [16] Hao, F., Zou, H.Y., Gong, Z.S., et al., 2007. Petroleum Migration and Accumulation in the Bozhong Sub-Basin, Bohai Bay Basin, China: Significance of Preferential Petroleum Migration Pathways (PPMP) for the Formation of Large Oilfields in Lacustrine Fault Basins. Marine and Petroleum Geology, 24: 1-13. doi: 10.1016/j.marpetgeo.2006.10.007 [17] He, L.J., Wang, J.Y., 2003. Cenozoic Thermal History of the Bohai Bay Basin: Constraints from Heat Flow and Coupled Basin-Mountain Modeling. Physics and Chemistry of the Earth, 28: 421-429. doi: 10.1016/S1474-7065(03)00062-7 [18] He, S.B., Zhu, W.L., Li, L.X., 2001. Sedimentary Evolution and Neogene Reservoir-Seal Assemblage Analysis of Bozhong Depression. Acta Petrolei Sinica, 22(2): 38-43(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYXB200102007.htm [19] Hindle, A.D., 1997. Petroleum Migration Pathway and Charge Concentration: A Three-Dimensional Model. AAPG Bulletin, 81(9): 1451-1481. [20] Hooper, E.C.D., 1991. Fluid Migration along Growth Faults in Compacting Sediments. Journal of Petroleum Geology, 14: 161-180. doi: 10.1111/j.1747-5457.1991.tb00360.x [21] Hu, S.B., O'Sullivan, P.B., Raza, A., et al., 2001. Thermal History and Tectonic Subsidence of the Bohai Basin, Northern China: A Cenozoic Rifted and Local Pull-Apart Basin. Physics of the Earth and Planetary Interiors, 126: 221-235. doi: 10.1016/S0031-9201(01)00257-6 [22] Jiang, F.J., Pang, X.Q., 2011. Quantitative Evaluation of Hydrocarbon Resource Potential and Its Distribution in the Bozhong Sag and Surrounding Areas, Bohai Bay Basin. Petroleum Exploration and Development, 38(1): 23-29(in Chinese with English abstract). doi: 10.1016/S1876-3804(11)60012-8 [23] Li, S.T., 2004. Basin Geodynamics Background of Formation of Huge Petroleum Systems. Earth Science—Journal of China University of Geosciences, 29(5): 505-512(in Chinese with English abstract). [24] Liang, S.Y., Liu, K.Q., Cai, Z.X., 2005. Study of Petroleum Accumulation System and Pathway System. Petroleum Geology and Experiment, 27(4): 327-332(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYSD200504002.htm [25] Liu, X.F., Xie, X.N., Zhang, C., 2008. Characteristics and Generation of the Reservoir Overpressure in Bozhong Depression, Bohai Bay Basin. Earth Science—Journal of China University of Geosciences, 33(3): 337-341(in Chinese with English abstract). doi: 10.3799/dqkx.2008.044 [26] Nie, F.J., Li, S.T., Wang, H., et al., 2001. Lateral Migration Pathways of Petroleum in the Zhu Ⅲ Sub-Basin, Pearl River Mouth Basin, South China Sea. Marine and Petroleum Geology, 18: 561-575. doi: 10.1016/S0264-8172(01)00013-7 [27] Pan, Z.X., 1983. The Significance of Unconformities for the Migration and Accumulation of Oil and Gas and Search for Some Oil and Gas Deposits below Unconformities. Geological Review, 29(4): 374-381(in Chinese with English abstract). [28] Rhea, L., Person, M., de Marsily, G., et al., 1994. Geostatistical Models of Secondary Oil Migration within Heterogeneous Carrier Beds: A Theoretical Example. AAPG Bulletin, 78(12): 1679-1691. [29] Sweeney, J.J., Burnham, A.K., 1990. Evolution of a Simple Model of Vitrinite Reflectance Based on Chemical Kinetics. AAPG Bulletin, 74: 1559-1570. http://www.researchgate.net/publication/255005110_Evaluation_of_a_simple_model_of_vitrinite_reflectance_based_on_Chemical_kinetics [30] Wan, T.F., Wang, M.M., Yin, X.L., et al., 2004. Sealing Properties of Different Direction Faults in the Bohai Bay Area. Geoscience, 18(2): 157-163(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XDDZ200402002.htm [31] Wang, L.S., Liu, S.W., Xiao, W.Y., et al., 2002. Distribution Feature of Terrestrial Heat Flow Densities in the Bohai Basin, East China. Chinese Science Bulletin, 47: 857-862. doi: 10.1360/02tb9193 [32] Wang, P.R., Zhang, D.J., Song, F.Q., et al., 2004. The Comprehensive Geochemical Parameters for Distinguishing Three Sets of Source Rock in Bozhong Depression. China Offshore Oil and Gas, 16(3): 157-160(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZHSD200403002.htm [33] Xie, T.J., Pan, Z.Y., Yang, X.C., 1997. Pathway System and Driving Force of Hydrocarbon Migration. In: Gong, Z.S., Li, S.T., eds., Continental Margin Basin Analysis and Hydrocarbon Accumulation of the Northern South China Sea. Science Press, Beijing, 385-405 (in Chinese). [34] Xie, X.N., Cui, T., Müller, R.D., et al., 2007. Subsidence History and Forming Mechanism of Anomalous Tectonic Subsidence in the Bozhong Depression, Bohaiwan Basin. Science in China (Series D): Earth Sciences, 50(9): 1310-318. doi: 10.1007/s11430-007-0095-8 [35] Xie, X.N., Li, S.T., Hu, X.Y., et al., 1999. Conduit Systems and Formation Mechanism of Heat Fluids in Diapiric Belt of Yinggehai Basin, China. Science in China (Series D), 42(6): 561-571. doi: 10.1007/BF02877783 [36] Xu, J., Zhou, B.G., Ji, F.J., et al., 2011. A Primary Study on the Neotectonic Pattern of the Bohai Area in China. Acta Petrolei Sinica, 32(3): 442-449(in Chinese with English abstract). http://www.researchgate.net/publication/279588079_A_primary_study_on_the_neotectonic_pattern_of_the_Bohai_area_in_China [37] Xue, Y.A., Liu, T.H., Wang, Y.B., et al., 2007. Main Controlling Factors and Model of Natural Gas Accumulation in Bohai Bay Area. Petroleum Exploration and Development, 34(5): 521-528(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SKYK200705002.htm [38] Yang, D.B., Zhu, G.Y., Su, J., et al., 2012. Types of Conduit Systems of Petroliferous Basins in China and Evaluation of Their Effectiveness. Journal of Southwest Petroleum University (Science & Technology Edition), doi: http://dx.doi.org/10.3863/j.issn.1674-5086(in Chinese with English abstract). [39] Yang, Y.T., Xu, T.G., 2004. Hydrocarbon Habitat of the Offshore Bohai Basin, China. Marine and Petroleum Geology, 21: 691-708. doi: 10.1016/j.marpetgeo.2004.03.008 [40] Yu, C.L., Zeng, J.H., 2005. Features of Fluid Migration and Hydrocarbon Accumulation in the Active and Intermittent Stages of Fault Episodic Activities. Petroleum Geology & Experiment, 27(2): 129-133 (in Chinese with English abstract). [41] Zhang, C., Xie, X.N., Jiang, T., et al., 2006. Hydrocarbon Migration and Accumulation along a Long-Term Growth Fault: Example from the BZ25-1 Oilfield of Bohai Basin, Eastern China. Journal of Geochemical Exploration, 89(1-3): 460-464. doi: 10.1016/j.gexplo.2005.11.032 [42] Zhang, G.C., Liu, Z.G., Chen, X.D., et al., 2001. Hydrocarbon Reservoir-Seal Combinations and Play Types in Bohai Sea. China Offshore Oil and Gas (Geology), 15(1): 29-34(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-ZHSD200101005.htm [43] Zhao, Z.X., Wang, H., Guo, Q.J., 2002. Types of Passage System and Analysis of Evolution of Its Capabilities in Temporal and Spatial Range. Petroleum Geology & Experiment, 24(6): 527-732(in Chinese with English abstract). http://www.cqvip.com/QK/95265X/200206/7443045.html [44] Zhu, W.L., Wang, G.C., Zhou, Y., 2000. Analysis of Petroleum Resource in Bohai Sea. Acta Petrolei Sinica, 21(3): 1-7 (in Chinese with English abstract). [45] Zhuo, Q.G., Ning, F.X., Rong, N., 2005. Types of Passage Systems and Reservoir-Controlling Mechanisms in Rift Basins. Geological Review, 51(4): 416-422 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP200504009.htm [46] Zou, H.Y., Hao, F., Zhang, B.Q., et al., 2005. Fluid-Conduit Framework and Its Control on Petroleum Accumulation in the Junggar Basin. Earth Science—Journal of China University of Geosciences, 30(5): 609-616 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200505013.htm [47] Zou, H.Y., Gong, Z.S., Teng, C.Y., et al., 2011. Late-Stage Rapid Accumulation of the PL19-3 Giant Oilfield in an Active Fault Zone during Neotectonism in the Bozhong Depression, Bohai Bay. Science China: Earth Sciences, 54(3): 388-398. doi: 10.1007/s11430-010-4144-3 [48] 邓运华, 1999. 渤海湾盆地凹陷—凸起油气聚集的差异性. 中国海上油气(地质), 13(6): 401-405. https://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD199906004.htm [49] 邓运华, 2005. 断裂-砂体形成油气运移的"中转站"模式. 中国石油勘探, 10(6): 14-18. doi: 10.3969/j.issn.1672-7703.2005.06.003 [50] 邓运华, 徐长贵, 李建平, 2011. 渤海大油田形成条件探讨. 中国工程科学, 13(5): 10-15. doi: 10.3969/j.issn.1009-1742.2011.05.002 [51] 龚再升, 王国纯, 2001. 渤海新构造运动控制晚期油气成藏. 石油学报, 22(2): 1-7. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB200102000.htm [52] 龚再升, 王国纯, 贺清, 2000. 上第三系是渤中坳陷及其周围油气勘探的主要领域. 中国海上油气(地质), 14(3): 145-156. https://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD200003000.htm [53] 郝芳, 蔡东升, 邹华耀, 等, 2004. 渤中坳陷超压-构造活动联控型流体活动与油气快速成藏. 地球科学——中国地质大学学报, 29(5): 518-524. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200405002.htm [54] 何仕斌, 朱伟林, 李丽霞, 2001. 渤中坳陷沉积演化和上第三系储盖组合分析. 石油学报, 22(2): 38-43. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB200102007.htm [55] 姜福杰, 庞雄奇, 2011. 环渤中凹陷油气资源潜力与分布定量评价. 石油勘探与开发, 38(1): 23-29. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201101005.htm [56] 李思田, 2004. 大型油气系统形成的盆地动力学背景. 地球科学——中国地质大学学报, 29(5): 505-512. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200405000.htm [57] 梁书义, 刘克奇, 蔡忠贤, 2005. 油气成藏体系及油气输导子体系研究. 石油实验地质, 27(4): 327-332. doi: 10.3969/j.issn.1001-6112.2005.04.003 [58] 刘晓峰, 解习农, 张成, 2008. 渤海湾盆地渤中坳陷储层超压特征与成因机制. 地球科学——中国地质大学学报, 33(3): 337-341. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200803007.htm [59] 潘钟祥, 1983, 不整合对于油气运移聚集的重要性及寻找不整合面下的某些油气藏. 地质论评, 29(4): 374-381. doi: 10.3321/j.issn:0371-5736.1983.04.008 [60] 万天丰, 王明明, 殷秀兰, 等, 2004. 渤海湾地区不同方向断裂带的封闭性. 现代地质, 18(2): 157-163. doi: 10.3969/j.issn.1000-8527.2004.02.003 [61] 王培荣, 张大江, 宋孚庆, 等, 2004. 区分渤中坳陷三套烃源岩的地球化学参数组合. 中国海上油气, 16(3): 157-160. doi: 10.3969/j.issn.1673-1506.2004.03.003 [62] 谢泰俊, 潘祖荫, 杨学昌, 1997. 油气运移动力及通道体系. 见: 龚再升, 李思田, 主编. 南海北部大陆边缘盆地分析与油气聚集. 北京: 科学出版社, 385-405. [63] 徐杰, 周本刚, 计凤桔, 等, 2011. 渤海地区新构造格局. 石油学报, 32(3): 442-449. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB201103009.htm [64] 薛永安, 刘廷海, 王应斌, 等, 2007. 渤海海域天然气成藏主控因素与成藏模式. 石油勘探与开发, 34(5): 521-528. doi: 10.3321/j.issn:1000-0747.2007.05.002 [65] 杨德彬, 朱光有, 苏劲, 等, 2012. 中国含油气盆地输导体系类型及其有效性评价. 西南石油大学学报(自然科学版), doi: 10.3863/j.issn.1674-5086. [66] 于翠玲, 曾溅辉, 2005. 断层幕式活动期和间歇期流体运移与油气成藏特征. 石油实验地质, 27(2): 129-133. doi: 10.3969/j.issn.1001-6112.2005.02.006 [67] 张功成, 刘志国, 陈晓东, 等, 2001. 渤海海域油气勘探组合与区带类型. 中国海上油气(地质), 15(1): 29-34. https://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD200101005.htm [68] 赵忠新, 王华, 郭齐军, 等, 2002. 油气输导体系的类型及其输导性能在时空上的演化分析. 石油实验地质, 24(6): 527-532. doi: 10.3969/j.issn.1001-6112.2002.06.009 [69] 朱伟林, 王国纯, 周毅, 2000. 渤海油气资源浅析. 石油学报, 21(3): 1-7. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB200003000.htm [70] 卓勤功, 宁方兴, 荣娜, 2005. 断陷盆地输导体系类型及控藏机制. 地质论评, 51(4): 416-422. doi: 10.3321/j.issn:0371-5736.2005.04.008 [71] 邹华耀, 郝芳, 张柏桥, 等, 2005. 准噶尔盆地流体输导格架及其对油气成藏与分布的控制. 地球科学——中国地质大学学报, 30(5): 609-616. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200505013.htm -
下载:
点击查看大图
图(9)
计量
- 文章访问数: 3240
- HTML全文浏览量: 100
- PDF下载量: 553
- 被引次数: 0
