川西前陆盆地侏罗系沉积体系变迁及演化模式

doi:10.7623/syxb201606005

石油学报 ›› 2016, Vol. 37 ›› Issue (6): 743-756.DOI: 10.7623/syxb201606005

川西前陆盆地侏罗系沉积体系变迁及演化模式

刘君龙¹, 纪友亮¹, 张克银², 李龙迪¹, 王天云¹, 杨永³, 张洁³

1. 中国石油大学地球科学学院油气资源与探测国家重点实验室北京 102249;
2. 中国石油化工股份有限公司西南分公司四川成都 610081;
3. 中国石油天然气勘探开发公司勘探部北京 100034

收稿日期:2015-09-23 修回日期:2016-03-10 出版日期:2016-06-25 发布日期:2016-06-30
通讯作者: 纪友亮,男,1962年10月生,1983获华东石油学院学士学位,1991年获石油大学(北京)博士学位,现为中国石油大学(北京)教授、博士生导师,主要从事石油地质学、沉积学和层序地层学方面的研究。Email:ji_youliang@sina.com
作者简介:刘君龙,男,1988年5月生,2011年获中国石油大学(华东)地质学专业学士学位,现为中国石油大学(北京)博士研究生,主要从事沉积学、石油地质学方向研究。Email:jl_liu2007@sina.cn
基金资助:
国家自然科学基金项目(No.41272157)、中国石油天然气集团公司科技创新基金项目(2014D-5006-0101)、中国石油大学(北京)科研基金项目(2462013YJRC038,2462015YQ0108)和国家重大科技专项(2011ZX05003-002)资助。

Jurassic sedimentary system transition and evolution model in Western Sichuan Foreland Basin

Liu Junlong¹, Ji Youliang¹, Zhang Keyin², Li Longdi¹, Wang Tianyun¹, Yang Yong³, Zhang Jie³

1. College of Geosciences, State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102249, China;
2. Sinopec Southwest Oil & Gas Company, Sichuan Chengdu 610081, China;
3. CNODC Exploration Department, Beijing 100034, China

Received:2015-09-23 Revised:2016-03-10 Online:2016-06-25 Published:2016-06-30

摘要/Abstract

摘要：

川西前陆盆地侏罗系整体气候炎热、干旱,受板块差异挤压的影响,周围山体继承性隆升,前渊坳陷不断发生迁移。构造作用控制物源区迁移,进一步分配了不同时期沉积体系的展布。通过大量野外露头、测-录井、岩心和分析化验资料,阐明了川西前陆盆地物源特征及沉积体系变迁,以塔里木盆地北缘现代沉积为启示,建立了川西前陆盆地沉积演化模式。结果表明:①这一时期,研究区主要发育2种类型沉积体系,分别为早侏罗世的冲积扇-河流-正常三角洲-湖泊沉积体系和中-晚侏罗世的冲积扇-河流-浅水三角洲-湖泊沉积体系;②早侏罗世,前陆盆地的前渊坳陷位于米仓山山前,短轴方向的龙门山主体是研究区的主要物源区;中侏罗世,前陆盆地的前渊坳陷转移到大巴山山前,长轴方向的大巴山和短轴方向龙门山主体共同为研究区供源;晚侏罗世,前陆盆地的前渊坳陷再次转移到龙门山北段山前,长轴方向的龙门山北段和短轴方向龙门山主体共同为研究区供源;③证实了"长轴短轴共存,近源远源汇砂"的物源分布特征,建立了2种川西侏罗纪前陆盆地沉积演化模式,分别为早侏罗世的再生前陆盆地大盆深湖模式和中-晚侏罗世的再生前陆盆地大盆小湖模式。

关键词: 物源体系, 沉积变迁, 演化模式, 侏罗系, 川西前陆盆地

Abstract:

During Jurassic sedimentary period, the climate of Western Sichuan Foreland Basin was hot and arid. Influenced by differential squeezing of the plates, surrounding mountains uplifted successively, and foredeep depression migrated continuously. Tectonism was able to control the migration of provenance area, further determining the distribution of sedimentary system in different periods. Based on a large number of field outcrop, logging, core and assay data, this study illustrates the provenance characteristics and sedimentary system transition of Western Sichuan Foreland Basin. Meanwhile, the sedimentary evolution model of Western Sichuan Foreland Basin is established by gaining enlightenment from the modern sedimentation on the northern margin of Tarim Basin. The results show that:(1) in this period, two types of sedimentary systems were primarily developed in the study area, i.e., Early Jurassic alluvial fan-fluvio-normal delta-lake sedimentary system and Mid-Late Jurassic alluvial fan-fluvio-shallow delta-lake sedimentary system. (2) In the Early Jurassic, the foredeep depression of Foreland Basin was located in front of Micang mountain, where Longmen mountain massif in the short axis acted as the main provenance area; in the Middle Jurassic, the foredeep depression of Foreland Basin migrated to the front of Daba mountain, where Daba mountain in the long axis and Longmen mountain massif in the short axis were major provenance areas of the study area; in the Late Jurassic, the foredeep depression of Foreland Basin migrated to the front of the northern segment of Longmen mountain again, where the northern segment of Longmen mountain in the long axis and Longmen mountain massif in the short axis were major provenance areas of the study area. (3) The provenance distribution characteristics, i. e., "coexistence of long axis and short axis, sand convergence of near source and far source", were confirmed. On this basis, this study establishes two Jurassic sedimentary evolution models of Western Sichuan Foreland Basin, i. e., large basin-deep lake model in the Early Jurassic rejuvenated foreland basin and large basin-small lake model in the Mid-Late Jurassic rejuvenated foreland basin.

Key words: provenance system, sedimentary migration, evolution model, Jurassic, Western Sichuan Foreland Basin

中图分类号:

TE121.3

刘君龙, 纪友亮, 张克银, 李龙迪, 王天云, 杨永, 张洁. 川西前陆盆地侏罗系沉积体系变迁及演化模式[J]. 石油学报, 2016, 37(6): 743-756.

Liu Junlong, Ji Youliang, Zhang Keyin, Li Longdi, Wang Tianyun, Yang Yong, Zhang Jie. Jurassic sedimentary system transition and evolution model in Western Sichuan Foreland Basin[J]. Acta Petrolei Sinica, 2016, 37(6): 743-756.

参考文献

[1] DeCelles P G,Giles K A.Foreland basin systems[J].Basin Research,1996,8(2):105-123.
[2] Jordan T E.Thrust loads and foreland basin evolution,Cretaceous,western United States[J].AAPG Bulletin,1981,65(12):2506-2520.
[3] Catuneanu O.Retroarc foreland systems-evolution through time[J].Journal of African Earth Sciences, 2004,38(3):225-242.
[4] Salvany J M,Larrasoaña J C,Mediavilla C,et al.Chronology and tectono-sedimentary evolution of the Upper Pliocene to Quaternary deposits of the Lower Guadalquivir foreland basin,SW Spain[J].Sedimentary Geology,2011,241(1/4):22-39.
[5] 贾承造,宋岩,魏国齐,等.中国中西部前陆盆地的地质特征及油气聚集[J].地学前缘,2005,12(3):3-13.
Jia Chengzao,Song Yan,Wei Guoqi,et al.Geological features and petroleum accumulation in the foreland basins in central and western China[J].Earth Science Frontiers,2005,12(3):3-13.
[6] 林畅松,刘景彦,张燕梅,等.库车坳陷第三系构造层序的构成特征及其对前陆构造作用的响应[J]. 中国科学:D辑,2002,32(3):177-183.
Lin Changsong,Liu Jingyan,Zhang Yanmei,et al.Depositional architecture of the Tertiary tectonic sequences and their response to foreland tectonism in the Kuqa depression,the Tarim Basin[J].Science in China:Series D,2002,45(3):250-258.
[7] 郑荣才,朱如凯,翟文亮,等.川西类前陆盆地晚三叠世须家河期构造演化及层序充填样式[J].中国地质,2008,35(2):246-255.
Zheng Rongcai,Zhu Rukai,Zhai Wenliang,et al.Tectonic evolution and sequence filling patterns in the western Sichuan foreland-like basin in the Upper Triassic Xujiahean period[J].Geology in China,2008,35(2):246-255.
[8] Anthony E J,Julian M.Source-to-sink sediment transfers,environmental engineering and hazard mitigation in the steep Var River catchment,French Riviera,southeastern France[J].Geomorphology,1999,31(1/4):337-354.
[9] Sømme T O,Helland-Hansen W,Martinsen O J,et al.Relationships between morphological and sedimentological parameters in source-to-sink systems:a basis for predicting semi-quantitative characteristics in subsurface systems[J].Basin Research,2009,21(4):361-387.
[10] 林畅松,夏庆龙,施和生,等.地貌演化、源-汇过程与盆地分析[J].地学前缘,2015,22(1):9-20.
Lin Changsong,Xia Qinglong,Shi Hesheng,et al.Geomorphological evolution,source to sink system and basin analysis[J].Earth Science Frontiers,2015,22(1):9-20.
[11] 刘和甫.前陆盆地类型及褶皱-冲断层样式[J].地学前缘,1995,2(3/4):59-68.
Liu Hefu.Classification of foreland basins and fold thrust style[J].Earth Science Frontiers,1995,2(3/4):59-68.
[12] 邓康龄.四川盆地形成演化与油气勘探领域[J].天然气工业,1992,12(5):7-12.
Deng Kangling.Formationand evolution of Sichuan basin and domains for oil and gas exploration[J].Natural Gas Industry,1992,12(5):7-12.
[13] 罗启后.安县运动对四川盆地中西部上三叠统地层划分对比与油气勘探的意义[J].天然气工业,2011,31(6):21-27.
Luo Qihou.Significance of the Anxian Movement to the stratigraphic division and correlation of the Upper Triassic formations and their hydrocarbon exploration in the western-central Sichuan basin[J].Natural Gas Industry,2011,31(6):21-27.
[14] 陈竹新,贾东,魏国齐,等.川西前陆盆地中-新生代沉积迁移与构造转换[J].中国地质,2008,35(3):472-481.
Chen Zhuxin,Jia Dong,Wei Guoqi,et al.Meso-Cenozoic sediment transport and tectonic transition in the western Sichuan foreland basin[J].Geology in China,2008,35(3):472-481.
[15] 徐胜林,侯明才,林良彪,等.川西前陆盆地侏罗纪构造层序地层格架内沉积充填特征[J].岩石学报,2011,27(8):2327-2338.
Xu Shenglin,Hou Mingcai,Lin Liangbiao,et al.Depositional characteristics within tectonic sequence of Jurassic,western Sichuan foreland basin[J].Acta Petrologica Sinica,2011,27(8):2327-2338.
[16] 安红艳,时志强,张慧娟,等.川西坳陷中段中侏罗统沙溪庙组储层砂岩物源分析[J].四川地质学报,2011,31(1):29-33.
An Hongyan,Shi Zhiqiang,Zhang Huijuan,et al.On material source of sandstone reservoir of the Middle Jurassic Shaximiao formation in west Sichuan depression[J].Acta Geologica Sichuan,2011,31(1):29-33.
[17] 李英强,何登发.四川盆地及邻区早侏罗世构造-沉积环境与原型盆地演化[J].石油学报,2014,35(2):219-232.
Li Yingqiang,He Dengfa.Evolution of tectonic-depositional environment and prototype basins of the Early Jurassic in Sichuan Basin and adjacent areas[J].Acta Petrolei Sinica,2014,35(2):219-232.
[18] 李智武,刘树根,林杰,等.川西坳陷构造格局及其成因机制[J].成都理工大学学报:自然科学版,2009,36(6):645-653.
Li Zhiwu,Liu Shugen,Lin Jie,et al.Structural configuration and its genetic mechanism of the west Sichuan depression in China[J].Journal of Chengdu University of Technology:Science & Technology Edition,2009,36(6):645-653.
[19] 杨运会,刘军,赵永华,等.洛带气田蓬莱镇组层序格架下的沉积相研究[J].天然气技术,2010,4(1):21-23.
Yang Yunhui,Liu Jun,Zhao Yonghua,et al.Sedimentary facies in a sequence stratigraphic framework of Penglaizhen Formation,Luodai gasfield[J].Natural Gas Technology,2010,4(1):21-23.
[20] 刘君龙,杨克明,纪友亮,等.川西坳陷上侏罗统浅水漫湖沉积特征与砂体叠置模式[J].古地理学报,2015,17(4):503-516.
Liu Junlong,Yang Keming,Ji Youliang,et al.Sedimentary characteristics and sand-body superposed patterns of flood-overlake deposits of the Upper Jurassic in Chuanxi depression[J].Journal of Palaeogeography,2015,17(4):503-516.
[21] 刘君龙,纪友亮,杨克明,等.浅水湖盆三角洲岸线控砂机理与油气勘探意义——以川西坳陷中段蓬莱镇组为例[J].石油学报,2015,36(9):1060-1073.
Liu Junlong,Ji Youliang,Yang Keming,et al.Mechanism of lake shoreline control on shoal water deltaic sandbodies and its significance for petroleum exploration:a case study of Penglaizhen Formation in the middle part of western Sichuan depression[J].Acta Petrolei Sinica,2015,36(9):1060-1073.
[22] 冯增昭.中国沉积学[M].第2版.北京:石油工业出版社,2013:743-746.
Feng Zengzhao.Sedimentology of China[M].2nd ed.Beijing:Petroleum Industry Press,2013:743-746.
[23] 邹才能,赵文智,张兴阳,等.大型敞流坳陷湖盆浅水三角洲与湖盆中心砂体的形成与分布[J].地质学报,2008,82(6):813-825.
Zou Caineng,Zhao Wenzhi,Zhang Xingyang,et al.Formation and distribution of shallow-water deltas and central-basin sandbodies in large open depression lake basins[J].Acta Geologica Sinica,2008,82(6):813-825.
[24] 朱筱敏,刘媛,方庆,等.大型坳陷湖盆浅水三角洲形成条件和沉积模式:以松辽盆地三肇凹陷扶余油层为例[J].地学前缘,2012,19(1):89-99.
Zhu Xiaomin,Liu Yuan,Fang Qing,et al.Formation and sedimentary model of shallow delta in large-scale lake,example from Cretaceous Quantou Formation in Sanzhao sag,Songliao Basin[J].Earth Science Frontiers,2012,19(1):89-99.
[25] 袁静.济阳坳陷南部古近系洪水-漫湖沉积[J].中国地质,2005,32(4):131-138.
Yuan Jing.Paleogene flooded lake sediments in the southern part of the Jiyang depression[J].Geology in China,2005,32(4):131-138.
[26] Beaumont C.Foreland basins[J].Geophysical Journal of the Royal Astronomical Society,1981,65(2):201-239.
[27] Clevis Q,De Boer P L,Nijman W.Differentiating the effect of episodic tectonism and eustatic sea-level fluctuations in foreland basins filled by alluvial fans and axial deltaic systems:insights from a three-dimensional stratigraphic forward model[J].Sedimentology,2004,51(4):809-835.
[28] 李智武,刘树根,陈洪德,等.龙门山冲断带分段-分带性构造格局及其差异变形特征[J].成都理工大学学报:自然科学版,2008,35(4):440-454.
Li Zhiwu,Liu Shugen,Chen Hongde,et al.Structural segmentation and zonation and differential deformation across and along the Lomgmen thrust belt,West Sichuan,China[J].Journal of Chengdu University of Technology:Science & Technology Edition,2008,35(4):440-454.
[29] 金文正,汤良杰,杨克明,等.龙门山冲断带构造特征研究主要进展及存在问题探讨[J].地质论评,2008,54(1):37-46.
Jin Wenzheng,Tang Liangjie,Yang Keming,et al.Progress and problem of study on characters of the Longmen Mountain Thrust Belt[J].Geological Review,2008,54(1):37-46.
[30] 周康,王强,乔永亮.龙门山造山带与川西前陆盆地的盆山耦合关系对油气成藏的控制作用[J].地球科学与环境学报,2011,33(4):378-383.
Zhou Kang,Wang Qiang,Qiao Yongliang.Control of the basin-range coupling relationship between Longmen Mountain Orogenic Belt and Western Sichuan foreland basin to hydrocarbon accumulation[J].Journal of Earth Sciences and Environment,2011,33(4):378-383.
[31] 钱利军.川西北地区中、下侏罗统物质分布规律与沉积充填过程[D].成都:成都理工大学,2013.
Qian Lijun.Regulation of sedimentary distribution and sedimentary filling process during Middle and Lower Jurassic in Western and Northern Sichuan,China[D].Chengdu:Chengdu University of Technology,2013.
[32] 邓宾.四川盆地中-新生代盆-山结构与油气分布[D].成都:成都理工大学,2013.
Deng Bin.Meso-Cenozoic architecture of basin-mountain system in the Sichuan Basin and its gas distribution[D].Chengdu:Chengdu University of Technology,2013.
[33] 孙东.米仓山构造带构造特征及中-新生代构造演化[D].成都:成都理工大学,2011.
Sun Dong.The structural character and Meso-Cenozoic evolution of Micang Mountain Structural Zone,Northern Sichuan Basin,China[D].Chengdu:Chengdu University of Technology,2011.
[34] 孙东,刘树根,邓宾,等.米仓山与龙门山接合部叠加褶皱特征及构造演化[J].成都理工大学学报:自然科学版, 2011,38(2):156-168.
Sun Dong,Liu Shugen,Deng Bin,et al.Superposed fold characteristics and structural evolution in the junction area of Longmenshan Mountains and Micangshan Mountains in the southwest of China[J].Journal of Chengdu University of Technology:Science & Technology Edition,2011,38(2):156-168.
[35] 谢志良,刘树根,赵磊,等.米仓山与龙门山结合部构造分带性特征[J].四川地质学报,2012,32(4):385-388.
Xie Zhiliang,Liu Shugen,Zhao Lei,et al.Tectonic Zonation in the junction of the Micang Mts with the Longmen Mts[J].Acta Geologica Sichuan,2012,32(4):385-388.
[36] Baltzer F,Purser B H.Modern alluvial fan and deltaic sedimentation in a foreland tectonic setting:the Lower Mesopotamian Plain and Arabian Gulf[J].Sedimentary Geology,1990,67(3/4):175-197.
[37] Ori G G.Continental depositional systems of the Quaternary of the Po Plain (northern Italy)[J].Sedimentary Geology,1993,83(1/2):1-14.
[38] Sinha R,Friend P F.River systems and their sediment flux,Indo-Gangetic plains,northern Bihar,India[J].Sedimentology,1994,41(4):825-845.
[39] Jin Jiuqiang,Aigner T,Luterbacher H P,et al.Sequence stratigraphy and depositional history in the south-eastern German Molasse Basin[J].Marine and Petroleum Geology,1995,12(8):929-940.
[40] Schlunegger F,Jordan T E,Klaper E M.Controls of erosional denudation in the orogen on foreland basin evolution:the Oligocene central Swiss Molasse basin as an example[J].Tectonics,1997,16(5):823-840.
[41] Nijman W.Cyclicity and basin axis shift in a piggyback basin:towards modelling of the Eocene Tremp-Ager Basin,South Pyrenees,Spain[M]//Mascle A,Puigdefàbregas C,Luterbacher H P,et al.Cenozoic Foreland Basins of Western Europe.Geological Society,London,Special Publications,1998,134:135-162.
[42] Dreyer T,Corregidor J,Arbues P,et al.Architecture of the tectonically influenced Sobrarbe deltaic complex in the Ainsa Basin,northern Spain[J].Sedimentary Geology,1999,127(3/4):127-169.

川西前陆盆地侏罗系沉积体系变迁及演化模式

Jurassic sedimentary system transition and evolution model in Western Sichuan Foreland Basin

PDF

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	郭旭升, 魏志红, 魏祥峰, 刘珠江, 陈超, 王道军. 四川盆地侏罗系陆相页岩油气富集条件及勘探方向[J]. 石油学报, 2023, 44(1): 14-27.
[2]	王清华, 张荣虎, 杨宪彰, 余朝丰, 徐振平, 周露, 王珂, 张亮. 库车坳陷东部迪北地区侏罗系阿合组致密砂岩气勘探重大突破及地质意义[J]. 石油学报, 2022, 43(8): 1049-1064.
[3]	杨雪, 石学文, 朱逸青, 刘佳, 李怡, 何亮, 徐亮, 李彦佑, 陈瑶, 蒋佳玉. 四川盆地南部泸州地区凯迪阶—埃隆阶深水页岩沉积演化与有机质富集[J]. 石油学报, 2022, 43(4): 469-482.
[4]	刘宇, 朱筱敏, 张自力, 王彤, 杨棵, 刘兴周, 郭峰. 基于地震沉积学恢复断陷湖盆古水系及其演化过程——以辽河坳陷西部凹陷盘山洼陷沙河街组三段为例[J]. 石油学报, 2022, 43(2): 207-222.
[5]	史超群, 许安明, 魏红兴, 胡春雷, 张星, 张文, 莫涛, 张慧芳, 周露, 史玲玲, 朱文慧, 陈维力. 构造挤压对碎屑岩储层破坏程度的定量表征——以库车坳陷依奇克里克构造带侏罗系阿合组为例[J]. 石油学报, 2020, 41(2): 205-215.
[6]	郭召杰, 赵浩男, 张元元. 侧缘前陆构造带:一种前陆构造带的新类型——以龙门山为例[J]. 石油学报, 2020, 41(12): 1477-1489.
[7]	刘金水, 李树霞, 秦兰芝, 易琦, 陈晓东, 康世龙, 沈文超, 邵龙义. 东海盆地西湖凹陷古近系煤的生烃动力学[J]. 石油学报, 2020, 41(10): 1174-1187,1218.
[8]	刘刚, 卫延召, 陈棡, 贾开富, 龚德瑜, 王峰, 孙靖, 朱峰, 麻伟娇. 准噶尔盆地腹部侏罗系-白垩系次生油气藏形成机制及分布特征[J]. 石油学报, 2019, 40(8): 914-927.
[9]	刘刚, 卫延召, 罗鸿成, 陈棡, 龚德瑜, 王峰, 孙靖, 贾开富. 准噶尔盆地陆西地区石南13井区侏罗系三工河组砂体结构及控藏作用[J]. 石油学报, 2018, 39(9): 1006-1018.
[10]	范存辉, 李虎, 钟城, 秦启荣, 胡东风, 张羽, 何顺, 张玮. 川东南丁山构造龙马溪组页岩构造裂缝期次及演化模式[J]. 石油学报, 2018, 39(4): 379-390.
[11]	庞正炼, 陶士振, 张琴, 张天舒, 杨家静, 范建玮, 袁苗. 四川盆地侏罗系致密油二次运移机制与富集主控因素[J]. 石油学报, 2018, 39(11): 1211-1222.
[12]	钱宇, 王作栋, 张婷, 妥进才, 王晓锋, 王志勇, 徐永昌. 准噶尔盆地东部侏罗系烃源岩和天然气地球化学特征及低熟气勘探前景[J]. 石油学报, 2017, 38(1): 44-54.
[13]	姜振学, 李峰, 杨海军, 李卓, 刘洛夫, 陈磊, 杜忠明. 库车坳陷迪北地区侏罗系致密储层裂缝发育特征及控藏模式[J]. 石油学报, 2015, 36(S2): 102-111.
[14]	邹娟, 戴俊生, 张丹丹, 伍亚, 张艺, 田博. 构造活动强度划分断陷盆地构造区划——以饶阳凹陷为例[J]. 石油学报, 2014, 35(2): 294-302,384.
[15]	高小跃, 刘洛夫, 尚晓庆, 王英, 苏天喜, 戴琦雯. 塔里木盆地侏罗系泥页岩储层特征与页岩气成藏地质背景[J]. 石油学报, 2013, 34(4): 647-659.