沉积盆地“源-汇”系统研究新进展

doi:10.11743/ogg20170101

摘要/Abstract

摘要：

近年来，“源-汇”研究已逐渐成为沉积学领域颇为关注的重要课题。系统梳理了国内外“源-汇”系统研究取得的新进展，分析总结了沉积体系“源-汇”研究思路与多方法综合分析技术，并指出了“源-汇”系统研究未来的发展趋势。大陆边缘盆地沉积体系的“源-汇”研究集中于沉积事件的触发机制和沉积物的搬运过程，复杂陆相断陷盆地在储层预测方面创新形成了“源-汇”时空耦合控砂原理及相应的控砂模式。“源-汇”研究将多方法物源示踪分析应用于古源区恢复与古水系重建中。针对陆相断陷盆地局部物源背景下的“源-汇”系统，潜在剥蚀区的层序地层学精细研究恢复了隐伏物源区地质历史时期的真实面貌。“源-汇”系统要素的定量化表征与储层的定量预测正在逐步探索之中，建立从源到汇的定量响应关系是最终目的，而在“源-汇”系统定量化约束下的沉积过程模拟，为少井条件下储层预测提供了有力支持。重视物源体系研究、定量化储层预测、多学科、多方法融合、过程化与机制化研究，形成工业化应用标准是未来沉积体系“源-汇”研究的发展趋势。

关键词: 源-汇, 物源示踪, 时空耦合控砂原理, 局部物源, 定量化, 沉积模拟, 大陆边缘盆地, 陆相断陷盆地

Abstract:

The "Source-to-Sink" system has been the focus of sedimentology research in recent years.In this paper,new research advances of "Source-to-Sink" at home and abroad are systematically reviewed,research methods and multi-methods integrated analysis technologies of the "Source-to-Sink" system are summarized and research trends are predicted.The "Source-to-Sink" system in continental margin basins focuses on the drivers of sedimentary event and transportation process,while in complex continental rift basins,principle of temporal-spatial coupled "Source-to-Sink" sandstone control and corresponding sandstone distribution models have been innovatively established.The "Source-to-Sink" research also focuses on application of multiple methods in sediment tracing to reveal paleo-provenance and reconstruct paleo-drainage.For the "Source-to-Sink" system in a provenance of continental rift basins,detailed analysis of sequence stratigraphy in potential eroded zone recovers the initial features of disappeared provenance in geological history.Quantitative characterization of the elements in the "Source-to-Sink" system and quantitative reservoir prediction has been under study,and establishment of quantitative relationship from source to sink is the final purpose.Sedimentary process simulation under the quantitative constraint provides significant support to reservoir prediction in sparse wells conditions.The research trends of "Source-to-Sink" include the following aspects:to improve provenance system research,to experiment on quantitative reservoir prediction,to combine multiple subjects and methods,to emphasize on process and mechanism analysis,and to form industrial application standard.

Key words: Source-to-Sink, provenance tracing, principle of spatial-temporal coupled sandstone control, regional provenance, quantification, sedimentary simulation, continental margin basin, continental rift basin

中图分类号:

TE121.3

徐长贵,杜晓峰,徐伟,等. 沉积盆地“源-汇”系统研究新进展[J]. 石油与天然气地质, 2017, 38(1): 1-11. doi: 10.11743/ogg20170101 Xu Changgui,Du Xiaofeng,Xu Wei,et al. New advances of the “Source-to-Sink” system research in sedimentary basin[J]. Oil & Gas Geology, 2017, 38(1): 1-11. doi: 10.11743/ogg20170101

参考文献

[1] The earth science community.MARGINS Program Science Plans[R].America:MARGINS Office,2004.
[2] Alexander C,Walsh J,Orpin A.Modern sediment dispersal and accumulation on the outer Poverty continental margin[J].Marine Geology,2010,270:213-226.
[3] Berryman K,Marden M,Palmer A,et al.The post-glacial downcutting history in the Waihuka tributary of Waipaoa River,Gisborne district:Implications for tectonics and landscape evolution in the Hikurangi subduction margin,New Zealand[J].Marine Geology,2010,270,55-71.
[4] Carter L,Orpin A,Kuehl S.From mountain source to ocean sink-the passage of sediment across an active margin,Waipaoa Sedimentary System,New Zealand[J].Marine Geology,2010,270:1-10.
[5] Fuller I,Marden M.Rapid channel response to variability in sediment supply:cutting and filling of the Tarndale-Fan,Waipaoa catchment,New Zealand[J].Marine Geology,2010,270:45-54.
[6] Kniskern T,Kuehl S,Harris C,et al.Sediment accumulation patterns and fine-scale strata formation on the Waiapu River shelf,New Zealand[J].Marine Geology,2010,270,188-201.
[7] Marsaglia K,DeVaughn A,James D,et al.Provenance of fluvial terrace sediments within the Waipaoa sedimentary system and their importance to New Zealand source-to-sink studies[J].Marine Geology,2010,270:84-93.
[8] Miller A J,Kuehl S A.Shelf sedimentation on a tectonically-active margin:A modern sediment budget for Poverty continental shelf,New Zealand[J].Marine Geology,2010,270,175-187.
[9] Orpin A R,Carter L,Rogers,et al.Holocene sedimentary record from Lake Tutira:A template for upland watershed erosion proximal to the Waipaoa Sedimentary System,northeastern New Zealand[J].Marine Geology,2010,270,11-29.
[10] Page M J,Trustrum N A,Orpin A R,et al.Storm frequency and magnitude in response to Holocene climate variability,Lake Tutira,North-Eastern New Zealand[J].Marine Geology,2010,270,30-44.
[11] Pedley K L,Barnes P M,Pettinga,et al.Seafloor structural geomorphic evolution of the accretionary frontal wedge in response to seamount subduction,Poverty Indentation,New Zealand[J].Marine Geology,2010,270,119-138.
[12] Rose L E,Kuehl S A.Recent sedimentation patterns and facies distribution on the Poverty Shelf,New Zealand[J].Marine Geology,2010,270,160-174.
[13] Shao L.Detrital zircon provenance of the Paleogene syn-rift sediments in the northern South China Sea[J].Geochemistry,Geophysics,Geosystems,2016,17:255-269.
[14] Shi H,Xu C,Zhou Z,Ma C.Zircon U-Pb dating on granitoids from the northern South China Sea and its geotectonic relevance[J].Acta Geologica Sinica,2011,85(6):1359-1372.
[15] Wang C,Liang X,Xie Y,et al.Provenance of Upper Miocene to Quaternary sediments in the Yinggehai-Song Hong Basin,South China Sea:Evidence from detrital zircon U-Pb ages[J].Marine Geology,2014,355:202-217.
[16] Wang C,Liang X,Xie Y,et al.Late Miocene provenance change on the eastern margin of the Yinggehai-Song Hong Basin,South China Sea:evidence from U-Pb dating and Hf isotope analyses of detrital zircons[J].Marine and Petroleum Geology,2015,61:123-139.
[17] Wang Y M,Xu Q,Li D,et al.Late Miocene Red River submarine fan,northwestern South China Sea[J].Chinese Science Bulletin,2011,56(14):1488-1494.
[18] Wolinsky,M A,Swenson,J B,Litchfield,N,et al.Coastal progradation and sediment partitioning in the Holocene Waipaoa.Sedimentary System,New Zealand[J].Marine Geology,2010,270:94-107.
[19] 邵磊.珠江口及北部湾盆地泥岩地球化学特点[J].同济大学学报,2000,28(5):523-527. Shao Lei.Geochemical characteristic of mudstone and provenance analyses of the pearl basin and beibu-gulf basin[J].Journal of Tongji University,2000,28(5):523-527.
[20] Clift P D,Blusztajn J,Nguyen D A.Large-scale drainage capture and surface uplift in eastern Tibet-SW China before 24 Ma inferred from sediments of the Hanoi Basin,Vietnam[J].Geophysical Research Letters,2006,33(19):1-4.
[21] Hoang V L,Wu F Y,Clift P D,et al.Evaluating the evolution of the Red River system based on in situ U-Pb dating and Hf isotope analysis of zircons[J].Geochemistry,Geophysics,Geosystems,2009,10(11):292-310.
[22] 王英民,徐强,李冬,等.南海西北部晚中新世的红河海底扇[J].科学通报,2011,56(10):781-787.
[23] Wang Yingmin,Xu Qiang,Li Dong,et al.Late Miocene Red River submarine fan,northwestern South China Sea[J].Chinese Science Bulletin,2011,56(10):781-787.
[24] 赵梦,邵磊,梁建设,等.古红河沉积物稀土元素特征及其物源指示意义[J].地球科学——中国地质大学(武汉)学报,2013,38增刊(1):166-174. Zhao Meng,Shao Lei,Liang Jianshe,et al.REE character of sediment from the paleo-red river and its implication of provenance[J].Earth Science:Journal of China University of Geosciences,2013,38 suppl(1):166-174.
[25] Cao L,Jiang T,Wang Z,et al.Provenance of Upper Miocene sediments in the Yinggehai and Qiongdongnan basins,northwestern South China Sea:evidence from REE,heavy minerals and zircon U-Pb ages[J].Marine Geology,2015,361:136-146.
[26] 刘强虎.珠江口盆地恩平凹陷古近系恩平组物源体系及其对滩坝的控制[J].石油学报,2015,36(3):286-299. Liu Qianghu.Provenance systems and their control on the beach-bar of Paleogene Enping Formation,Enping sag,Pearl River Mouth Basin[J].Acta Petrolei Sinica,2015,36(3):286-299.
[27] 祝彦贺,朱伟林,徐强,等.珠江口盆地13.8Ma陆架边缘三角洲与陆坡深水扇的"源-汇"关系[J].中南大学学报(自然科学版),2011,42(12):3827-3834. Zhu Yanhe,Zhu Weilin,Xu Qiang,et al.Sedimentary response to shelf-edge delta and slope deep-water fan in 13.8 Ma of Miocene epoch in Pearl River Mouth Basin[J].Journal of Central South University(Science and Technology),2011,42(12):3827-3834.
[28] 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.
[29] 徐长贵.陆相断陷盆地源-汇时空耦合控砂原理:基本思想、概念体系及控砂模式[J].中国海上油气,2013,25(4):1-11. Xu Changgui.Controlling sand principle of source-sink coupling in time and space in continental rift basins:basic idea,conceptual systems and controlling sand models[J].China Offshore Oil and Gas,2013,25(4):1-11.
[30] Normark W R.Submarine canyons and fan valleys:factors affecting growth patterns of deep-sea fans[J].Modern and Ancient Geosynclinals Sedimentation,Tulsa:Spc.Publ.SOC.Econ.Paleont.Miner.,1974(19):26-68.
[31] Nardin T R,Hein F J,Gorsline D S,et al.A review of mass movement processes,sediment and acoustic characteristics,and contrasts in slope and base-of-slope systems vs.canyon-fan-basin floor systems[J].Geology of Continental Slopes.Tulsa:Spc.Publ.SOC.Econ.Paleont.Miner.,1979(19):61-73.
[32] 徐长贵,赖维成,薛永安,等.古地貌分析在渤海古近系储集层预测中的应用[J].石油勘探与开发,2004,31(5):53-56. Xu Changgui,Lai Weicheng,Xue Yongan,et al.Palaeo-geomorphology analysis for the Paleogene reservoir prediction in Bohai Sea area[J].Petroleum Exploration and Development,2004,31(5):53-56.
[33] 林畅松,潘元林,肖建新,等."构造坡折带"——断陷盆地层序分析和油气预测的重要概念[J].地球科学——中国地质大学学报,2000,25(3):260-266. Lin Changsong,Pan Yuanlin,Xiao Jianxin,et al.Structural slope-break zone:key concept for stratigraphic sequence analysis and petroleum forecasting in fault subsidence basins[J].Earth Science:Journal of China University of Geosciences,2000,25(3):260-266.
[34] 赵贤正,金凤鸣,刘震,等.二连盆地地层岩性油藏"多元控砂-四元成藏-主元富集"与勘探实践(Ⅰ)[J].岩性油气藏,2007,19(2):9-15. Zhao Xianzheng,Jin Fengming,Liu Zhen,et al."Multi-factor controlling,four-factor entrapping and key-factor enrichment" of stratigraphic-lithologic reservoir sand exploration practice in Erlian Basin(Ⅰ):"Multi-factor controlling" mechanism[J].Lithologic Reservoirs,2007,19(2):9-15.
[35] 冯有良,徐秀生.同沉积构造坡折带对岩性油气藏富集带的控制作用——以渤海湾盆地古近系为例[J].石油勘探与开发,2006,33(1):22-25. Feng Youliang,Xu Xiusheng.Syndepositional structural slope-break zone controls on lithologic reservoirs:A case from Paleogene Bohai Bay Basin[J].Petroleum Exploration and Development,2006,33(1):22-25.
[36] 王家豪,王华,肖敦清,等.伸展构造体系中传递带的控砂作用——储层预测的新思路[J].石油与天然气地质,2008,29(1):20-25. Wang Jiahao,Wang Hua,Xiao Dunqing,et al.Control of transfer zone on sand bodies in the extensional structure system:a new approach to reservoir prediction[J].Oil & Gas Geology,2008,29(1):20-25.
[37] 吴海波,李军辉,刘赫.海拉尔盆地呼和湖凹陷南屯组构造坡折带类型及其对砂体和油气的控制[J].沉积学报,2013,31(2):358-365. Wu Haibo,Li Junhui,Liu He.Types of structural slope-break zone and its controls on sand bodies and hydrocarbon of Huhehu depression in Hailar basin[J].Acta Sedimentologica Sinica,2013,31(2):358-365.
[38] 樊太亮,李卫东.层序地层应用于陆相油藏预测的成功实例[J].石油学报,1999,20(2):12-17. Fan Tailiang,Li Weidong.A successful case on sequence stratigraphy applied to the prediction of non marine oil reservoir[J].Acta Petrolei Sinica,1999,20(2):12-17.
[39] 李思田,潘元林,陆永潮,等.断陷湖盆隐蔽油藏预测及勘探的关键技术——高精度地震探测基础上的层序地层学研究[J].地球科学,2002,27(5):592-596. Li Sitian,Pan Yuanlin,Lu Yongchao,et al.Key technology of prospecting and exploration of subtle traps in lacustrine fault basins:sequence stratigraphic researches on the basis of high resolution seismic survey[J].Earth Science:Journal of China University of Geosciences,2002,27(5):592-596.
[40] 邓宏文,王红亮,王居峰,等.层序地层构成与层序控砂、控藏的自相似性特征——以三角洲、浊积扇体系为例[J].石油与天然气地质,2004,25(5):491-495. Deng Hongwen,Wang Hongliang,Wang Jufeng,et al.Self-similarity of constitution of sequence stratigraphy and distribution of sandbodies and lithologic reservoirs:taking delta-turbidite fan system as an example[J].Oil & Gas Geology,2004,25(5):491-495.
[41] 徐长贵.渤海古近系坡折带成因类型及其对沉积体系的控制作用[J].中国海上油气,2006,18(6):365-371. Xu Changgui.Genetic types of Paleogene slope-break zonesand their controls on depositionalsystem in Bohai offshore[J].China Offshore Oil and Gas,2006,18(6):365-371.
[42] Allen P A.From landscapes into geological history[J].Nature,2008,451,274-276.
[43] Dickinson W,Suczek C.Plate tectonics and sandstone compositions[J].AAPG Bulletin,1979,63(12):2164-2182.
[44] Rollinson H R.Using geochemical data:evaluation,presentation,interpretation[M].Longman,Singapore.1993.
[45] Morton A C,Hallsworth C R.Identifying provenance-specific features of detrital heavy mineral assemblages in sandstones[J].Sedimentary Geology,1994,90:241-256.
[46] Li Xianhua.Geochemical and Nd isotopic variations in the sediments of the South China Sea:a response to Cenozoic tectonism in SE Asian[J].Earth and Planetary Science Letters,2003,211:207-220.
[47] Liu Q.Provenance identification and sedimentary analysis of the beach and bar systems in the Palaeogene of the Enping Sag[J].Marine and Petroleum Geology,2016,70:251-272.
[48] Liu Z,Shi H,Zhu J,et al.Detrital K-feldspar 40Ar/39Ar ages:source constraints of the Lower Miocene sandstones in the Pearl River Mouth Basin,South China Sea[J].Acta Geologica Sinica,2012,86(2):383-392.
[49] Moecher D,Samson S.Differential zircon fertility of source terranes and natural bias in the detrital zircon record:implications for sedimentary provenance analysis[J].Earth and Planetary Science Letters,2006,247,252-266.
[50] Clark M K,Schoenbohm L M,Royden L H,et al.Surface uplift,tectonics and erosion of eastern Tibet from large-scale drainage patterns[J].Tectonics,2004,23:1-20.
[51] Clift P D,Lee J I,Clark M K,et al.Erosional response of south China to arc rifting and monsoonal strengthening; a record from the South China Sea[J].Marine Geology,2002,184,207-226.
[52] He M,Zheng H,Clift P D.Zircon U-Pb geochronology and Hf isotope data from the Yangtze River sands:Implications for major magmatic events and crustal evolution in Central China[J].Chemical Geology,2013,360-361:186-203.
[53] Hicks D M,Gomez B,Trustrum N A.Erosion thresholds and suspended sediment yields,Waipaoa River basin,New Zealand[J].Water Resources Research,2000,36,1129-1142.
[54] Hicks D M,Gomez B,Trustrum N A.Event suspended sediment characteristics and the generation of hyperpycnal plumes at river mouths:East Coast continental margin,North Island,New Zealand[J].Journal of Geology,2004,112,471-485.
[55] Jiang T.Insights from heavy minerals and zircon U-Pb ages into the middle Miocene-Pliocene provenance evolution of the Yinggehai Basin,northwestern South China Sea[J].Sedimentary Geology,2015,327:32-42.
[56] Yan Y,Carter A,Palk C,et al.Understanding sedimentation in the Song Hong-Yinggehai Basin,South China Sea[J].Geochemistry,Geophysics,Geosystems,2011,12.
[57] Zhao M,Shao L,Qiao P.No Red River capture since the late Oligocene:geochemical evidence from the northwestern South China Sea[J].Deep Sea ResearchⅡ,2015,122,185-194.
[58] Nie J.Integrated provenance analysis of a convergent retroarc foreland system:U-Pb ages,heavy mineral,Nd isotopes,and sandstone compositions of the Middle Magdalena Valley basin,northern Andes,Colombia[J].Earth-Science Reviews,2012,110:111-126.
[59] Lowe D,Sylvester P,Enachescu M.Provenance and paleodainage patterns of Upper Jurassic and Lower Cretaceous synrift[J].AAPG Bulletin,2011,95(8):1295-1320.
[60] 赖志云,周维.舌状三角洲和鸟足状三角洲形成以及演变的沉积模拟实验[J].沉积学报,1994,12(2):37-43. Lai Zhiyun,Zhou Wei.Experimental formation and development of lobate and birdfoot deltas[J].Acta Sedimentologica Sinica,1994,12(2):37-43.
[61] 刘忠保,施冬,谢锐杰,等.三角洲分流河道形成及演变模拟研究[J].矿物岩石,2000,20(3):53-58. Liu Zhongbao,Shi Dong,Xie Ruijie,et al.The simulation of the formation and evolution of the distributary channel of delta[J].Journal of Mineralogy and Petrology,2000,20(3):53-58.
[62] 刘忠保,龚文平,张春生,等.沉积物重力流砂体形成及分布的沉积模拟试验研究[J].石油天然气学报,2006,28(3):20-22. Liu Zhongbao,Gong Wenping,Zhang Chunsheng,et al.Experimental Study on Sedimentary Modeling on the Formation and Distribution of Gravity Flow Sandbody[J].Journal of Oil and Gas Technology,2006,28(3):20-22.
[63] 张春生,刘忠保,施冬,等.砂质扇三角洲沉积过程实验研究[J].江汉石油学院学报,2003,25(2):1-3. Zhang Chunsheng,Liu Zhongbao,Shi Dong,et al.Experimental study of sandy-fan-delta sedimentary process[J].Journal of Jianghan Petroleum Institute,2003,25(2):1-3.
[64] 王随继,薄俊丽.网状河流多重河道形成过程的实验模拟[J].地理科学进展,2004,23(3):34-42. Wang Suiji,Bo Junli.Experimental simulation of anastomosing multiple channel formation[J].Process in Geography,2004,23(3):34-42.
[65] 杨华,牛小兵,罗顺社,等.鄂尔多斯盆地陇东地区长7段致密砂体重力流沉积模拟实验研究[J].地学前缘,2015,22(3):322-332. Yang Hua,Niu Xiaobin,Luo Shunshe,et al.Research of simulated experiment on gravity flow deposites of tight sand bodies of Chang 4Formation in Longdong area,Ordos Basin[J].Earth Science Frontiers,2015,22(3):322-332.
[66] 吕明,王颖,徐徽.沉积模拟方法在Bonaparte盆地的应用[J].中国海上油气,2010,22(2):83-90. Lu Ming,Wang Ying,Xu Hui.An application of sedimentation simulation in Bonaparte basin[J].China Offshore Oil and Gas,2010,22(2):83-90.
[67] 庞雄奇.地质过程定量模拟[M].北京:石油工业出版社,2003:1-13. Pang Xiongqi.Quantitative simulation of geological processes[M].Beijing:Petroleum Industry Press,2003:1-13.
[68] Burton R,Kendall C G C,Lerche I.Out of our depth:On the impossibility of fathoming eustasy from the stratigraphic record[J].Earth-Science Reviews,1987,24:237-277.
[69] 刘晖,操应长,徐涛玉,等.沉积坡折带控砂的模拟实验研究[J].山东科技大学,2007,26(1):34-37. Liu Hui,Cao Yingchang,Xu Taoyu,et al.The simulation experiment about the control of sandybody in depositional slope-break belt[J].Journal of Shandong University of Science and Technology,2007,26(1):34-37.
[70] Kubo Y,Nakajima T.Laboratory experiments and numerical simulation of sediment-wave formation by turbidity currents[J].Marine Geology,2003,192(1):105-122.
[71] Van Heijst,Postma G.Fluvial response to sea-level changes:A quantitative analogue,experimental approach[J].Basin Research,2001,13:269-292.