季节性河流体系高流态沉积构造特征:以内蒙古岱海湖半滩子河为例<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2018.06.067

古地理学报 ›› 2018, Vol. 20 ›› Issue (6): 929-940. doi: 10.7605/gdlxb.2018.06.067

• “碎屑岩油气储层表征” 专辑 • 下一篇

季节性河流体系高流态沉积构造特征:以内蒙古岱海湖半滩子河为例^*

谭程鹏¹, 于兴河², 刘蓓蓓³, 许磊⁴, 李顺利², 冯双奇¹, 唐雨生¹

1 西南石油大学地球科学与技术学院,四川成都 610500;
2 中国地质大学(北京)能源学院,北京 100083;
3 中国石油大学(北京)地球科学学院,北京 102249;
4 中海油研究总院开发研究院,北京 100028

收稿日期:2018-04-04 修回日期:2018-04-30 出版日期:2018-12-01 发布日期:2018-11-27
通讯作者: 于兴河,男,1958年生,博士,中国地质大学(北京)教授,博士生导师,主要从事沉积学和油气储层表征研究。E-mail: billyu@cugb.edu.cn。
作者简介:谭程鹏,男,1988年生,现为西南石油大学地球科学与技术学院讲师,主要从事沉积学与储层地质学研究。E-mail: tcp_swpu@126.com。
基金资助:
*国家自然科学基金项目(编号: 41602117,41472091),国家科技重大专项(编号: 2017ZX05001-002)及国家海洋局海洋沉积与环境地质重点实验室开放基金项目(编号:MASEG201706)联合资助

Sedimentary structures formed under upper-flow-regime in seasonal river system: A case study of Bantanzi River,Daihai Lake, Inner Mongolia

Tan Cheng-Peng¹, Yu Xing-He², Liu Bei-Bei³, Xu Lei⁴, Li Shun-Li², Feng Shuang-Qi¹, Tang Yu-Sheng¹

1 School of Geoscience and Technology,Southwest Petroleum University,Chengdu 610500, Sichuan;
2 School of Energy Resources,China University of Geosciences(Beijing),Beijing 100083;
3 College of Geosciences,China University of Petroleum(Beijing),Beijing 102249;
4 CNOOC Research Institute,Beijing 100028;

Received:2018-04-04 Revised:2018-04-30 Online:2018-12-01 Published:2018-11-27
Contact: Yu Xing-He,born in 1958,is a professor of China University of Geoscience(Beijing). He is mainly engaged in researches of sedimentology and reservoir characterization. E-mail: billyu@cugb.edu.cn.
About author:Tan Cheng-Peng,born in 1988,is a lecturer of Southwest Petroleum University. He is mainly engaged in researches of sedimentology and reservoir geology. E-mail: tcp_swpu@126.com.
Supported by:
Co-funded by the National Natural Science Foundation of China(No.41602117,41472091), National Science and Technology Major Project(No.2017ZX05001-002) and Opening Foundation of the Key Laboratory of Marine Sedimentology & Environmental Geology SOA(No. MASEG201706)

摘要/Abstract

摘要： 高流态尤其是超临界流动的水动力学机制及其床沙底形演化的研究相较于次临界流动具有一定的差距。季节性河流以高流态为主要沉积搬运过程,为超临界流的形成与保存提供了有利条件,是研究超临界流沉积的重要载体。在季节性河流沉积体系研究进展调研基础上,明确了其基本定义、判别标准及沉积特征。通过对内蒙古岱海湖北部典型季节性冲积体系——半滩子河流发育的沉积构造进行研究表明:随着低流态向高流态演化,沙丘底形(Dune)逐步向上部平坦床沙底形(Upper plane bed)过渡,形成了低角度/S型交错层理;在高流态初期,形成了上部平坦床沙成因的平行层理;随着流动强度逐渐增大,流动机制演变为超临界流,平坦床沙逐渐向逆行沙丘(Antidune)过渡,形成了与平行层理伴生的逆行沙丘交错层理;当流动强度进一步增大,携带沉积物的流体发生较强的水力跳跃,形成了流槽与冲坑(Chute-and-Pool)。半滩子河流现代沉积中发育的高流态沉积与区域内气候变化具有明确的响应关系,表明河流沉积中广泛发育的高流态沉积构造指示了强烈季节性变化的气候特征。

关键词: 高流态, 季节性河流, 超临界流, 沉积构造, 气候响应, 岱海湖

Abstract: In contrast to Froude subcritical flows,understanding of the mechanism and genetic bedforms of upper-flow-regime,especially Froude supercritical flows,remains limited. Seasonal rivers have been considered as important proxy for the study of upper-flow-regime,since the highly potential of preservation and generation of bedforms produced under upper-flow-regime in this kind of depositional system. In this study,the definition,criterion and sedimentary characteristics of seasonal rivers have been summarized briefly according to literatures review. Upper-flow-regime sedimentary structures in the Bantanzi River,which is a typical seasonal alluvial system at the north margin of Daihai Lake,were identified and interpreted. Results show that low-angle and sigmoidal cross-stratifications were generated during the transformation period of dune to upper plane bed. At the initial stage of upper-flow-regime,planar laminations were formed by upper plane bed. As flow strength increasing,flow regime changed to supercritical flow and antidune cross-stratifications were produced. With consistent increasing in flow strength,hydraulic jumps arisen in sediment-laden flow,hence chute-and-pool occurred and produced related sedimentary structures. The upper-flow-regime sedimentary structures developed in the Bantanzi River correspond genetically to the climate features in this area,which infers that extensive upper-flow-regime structures produced and preserved in fluvial deposits could indicate strongly seasonal variation of paleoclimate.

Key words: upper-flow-regime, seasonal rivers, Froude supercritical flow, sedimentary structure, climate response, Daihai Lake

中图分类号:

P736.22

谭程鹏, 于兴河, 刘蓓蓓, 许磊, 李顺利, 冯双奇, 唐雨生. 季节性河流体系高流态沉积构造特征:以内蒙古岱海湖半滩子河为例^*[J]. 古地理学报, 2018, 20(6): 929-940.

Tan Cheng-Peng, Yu Xing-He, Liu Bei-Bei, Xu Lei, Li Shun-Li, Feng Shuang-Qi, Tang Yu-Sheng. Sedimentary structures formed under upper-flow-regime in seasonal river system: A case study of Bantanzi River,Daihai Lake, Inner Mongolia[J]. JOPC, 2018, 20(6): 929-940.

http://www.gdlxb.cn/CN/Y2018/V20/I6/929

参考文献

[1] 操应长,杨田,王艳忠,李文强. 2017. 超临界沉积物重力流形成演化及特征. 石油学报, 38(6): 607-621.
[Cao Y C,Yang T,Wang Y Z,Li W Q.2017. Formation,evolution and sedimentary characteristics of supercritical sediment gravity-flow. Acta Petrolei Sinica, 38(6): 607-621]
[2] 高志勇,冯佳睿,周川闽,崔京钢,李小陪,赵雪松,郭美丽,吴昊. 2014. 干旱气候环境下季节性河流沉积特征: 以库车河剖面下白垩统为例. 沉积学报, 32(6): 1060-1071.
[Gao Z Y,Feng J R,Zhou C M,Cui J G,Li X P,Zhao X S,Guo M L,Wu H.2014. Arid climate seasonal rivers deposition: A case of Lower Cretaceous in Kuche river outcrop. Acta Sedimentologica Sinica, 32(6): 1060-1071]
[3] 高志勇,周川闽,冯佳睿,崔京钢,郭美丽,吴昊. 2015. 盆地内大面积砂体分布的一种成因机理:干旱气候下季节性河流沉积. 沉积学报, 33(3): 427-438.
[Gao Z Y,Zhou C M,Feng J R, Cui J G,Guo M L,Wu H.2015. Distribution of a large area of sand body formation mechanism: Ephemeral streams in arid climate. Acta Sedimentologica Sinica, 33(3): 427-438]
[4] 李华启,姜在兴,邱隆伟,邓兴梁,赵少宇,鲁洪波. 2003. 柯克亚凝析气田中新统西河甫组季节性河流沉积特征研究. 新疆地质, 21(1): 69-73.
[Li H Q,Jiang Z X,Qiu L W,Deng X L,Zhao S Y,Lu H B.2003. Seasonal river sedimentation of Xihefu Formation in Kekeya gas condensate field. Xinjiang Geology, 21(1): 69-73]
[5] 于兴河. 2008. 碎屑岩系油气储层沉积学. 北京: 石油工业出版社,108-110.
[Yu X H.2008. Clastic Petroleum Reservoir Sedimentology. Beijing: Petroleum Industry Press,108-110]
[6] 于兴河,李胜利. 2009. 碎屑岩系油气储集层沉积学的发展历程与热点问题思考. 沉积学报, 27(5): 880-895.
[Yu X H,Li S L.2009. The development and hotspot problems of clastic petroleum reservoir sedimentology. Acta Sedimentologica Sinica, 27(5): 880-895]
[7] Alexander J,Bridge J S,Cheel R J,LeClair S F.2001. Bedforms and associated sedimentary structures formed under supercritical water flows over aggrading sand beds. Sedimentology, 48(1): 133-152.
[8] Alexander J,Fielding C R.1997. Gravel antidunes in the tropical Burdekin River,Queensland,Australia. Sedimentology, 44(2): 327-337.
[9] Allen J P,Fielding C R,Rygel M C.2013. Deconvolving signals of tectonic and climatic controls from continental basins: An example from the Late Paleozoic Cumberland Basin,Atlantic Canada. Journal of Sedimentary Research, 83(9-10): 847-872.
[10] Allen J P,Fielding C R,Gibling M R,Rygel M C.2011. Fluvial response to paleoequatorial climate fluctuations during the late Paleozoic ice age. Geological Society of America Bulletin, 128(7-8): 1524-1538.
[11] Allen J P,Fielding C R,Gibling M R,Rygel M C.2014. Recognizing products of palaeoclimate fluctuation in the fluvial stratigraphic record: An example from the Pennsylvanian to Lower Permian of Cape Breton Island,Nova Scotia. Sedimentology, 61(5): 1332-1381.
[12] Banham S G,Mountney N P.2014. Climatic versus halokinetic control on sedimentation in a dryland fluvial succession. Sedimentology, 61(2): 570-608.
[13] Best J,Bridge J.1992. The morphology and dynamics of low amplitude bedwaves upon upper stage plane beds and the preservation of planar laminae. Sedimentology, 39(5): 737-752.
[14] Billi P.2007. Morphology and sediment dynamics of ephemeral stream terminal distributary systems in the Kobo Basin(northern Welo,Ethiopia). Geomorphology, 85(1): 98-113.
[15] Blair T C.1987. Sedimentary processes,vertical stratification sequences,and geomorphology of the Roaring River alluvial fan,Rocky Mountain National Park,Colorado. Journal of Sedimentary Petrology, 57(1): 1-18.
[16] Bridge J S.1981. Bed shear stress over subaqueous dunes,and the transition to upper stage plane beds. Sedimentology, 28(1): 33-36.
[17] Bridge J S,Best J L.1988. Flow,sediment transport and bedform dynamics over the transition from dunes to upper-stage plane beds: Implications for the formation of planar laminae. Sedimentology, 35(5): 753-763.
[18] Browne G H,Plint A G.1994. Alternating braidplain and lacustrine deposition in a strike-slip setting: The Pennsylvanian Boss Point Formation of the Cumberland Basin,Maritime Canada. Journal of Sedimentary Research, 64(1): 40-59.
[19] Calder J H.1998. The Carboniferous evolution of Nova Scotia. In: Blundell D J,Scott A C(eds). Charles Lyell: The Past is the key to the present. Special Publication of Geological Society of London, 143: 261-302.
[20] Carling P A,Schvidchenko A B.2002. A consideration of the dune-antidune transition in fine gravel. Sedimentology, 49(6): 1269-1282.
[21] Cartigny M J B,Ventra D,Postma G,Wagoner D B J H.2014. Morphodynamics and sedimentary structures of bedforms under supercritical-flow conditions: New insights from flume experiments. Sedimentology, 61(3): 712-748.
[22] Chakraborty T,Ghosh P.2010. The geomorphology and sedimentology of the Tista megafan,Darjeeling Himalaya: Implications for megafan building processes. Geomorphology, 115(3): 252-266.
[23] Cheel R J.1990. Horizontal lamination and the sequence of bed phases and stratification under upper-flow-regime conditions. Sedimentology, 37(3): 517-529.
[24] Chow V T.1959. Open-channel Hydraulics. McGraw-Hill Book,New York: 39-69.
[25] Coleman J M.1969. Brahmaputra River: Channel processes and sedimentation. Sedimentary Geology, 3(2): 129-239.
[26] Croke J C,Magee J M,Price D M.1998. Stratigraphy and sedimentology of the lower Neales River,West Lake Eyre,Central Australia: From Palaeocene to Holocene. Palaeogeography,Palaeoclimatology,Palaeoecology, 144(3-4): 331-350.
[27] Fielding C R.2006. Upper flow regime sheets,lenses and scour fills: Extending the range of architectural elements for fluvial sediment bodies. Sedimentary Geology, 190(1): 227-240.
[28] Fielding C R,Alexander J.1996. Sedimentology of the upper Burdekin River of north Queensland,Australia: An example of a tropical,variable discharge river. Terra Nova, 8(5): 447-457.
[29] Fielding C R,Webb J A.1996. Facies and cyclicity of the Late Permian Bainmedart Coal Measures in the northern Prince Charles Mountains,MacRobertson Land,Antarctica. Sedimentology, 43(2): 295-322.
[30] Fielding C R,Sliwa R,Holcombe R J,Kassan J.2000. A new palaeogeographic synthesis of the Bowen Basin of central Queensland. In: Beeston J (ed).Bowen Basin Symposium 2000 Proceedings. Geological Society of Australia Coal Geology Group,Rockhampton:287-302.
[31] Fielding C R,Allen J P,Alexander J,Gibling M R.2009. Facies model for fluvial systems in the seasonal tropics and subtropics. Geology, 37(7): 623-626.
[32] Friedman G M,Sanders J E.1978. Principles of Sedimentology. Wiley: 1-38.
[33] Fukuoka S,Okutsu K,Yamasaka M.1982. Dynamics and kinematic features of sand waves in upper regime. Proceeding of Japanese Society of Civil Engineering, 323: 77-89.
[34] Goodbred S L.2003. Response of the Ganges dispersal system to climate change: A source-to-sink view since the last interstade. Sedimentary Geology, 162(1): 83-104.
[35] Hasiotis S T,Wagoner J C,Demko T M,Wellner R W,Jones C R,Hill R E.2005. Continental ichnology: Using terrestrial and freshwater trace fossils for environmental and climatic interpretations. SEPM Short Course,51.
[36] Hinds D J,Aliyeva E,Allen M B,Davies C E,Kroonenberg S B,Simmons M D,Vincent S J.2004. Sedimentation in a discharge dominated fluvial-lacustrine system: The Neogene Productive Series of the South Caspian Basin,Azerbaijan. Marine and Petroleum Geology, 21(5): 613-638.
[37] Karcz I,Kersey D.1980. Experimental study of free surface flow instability and bedforms in shallow flows. Sedimentary Geology, 27(4): 263-300.
[38] Kennedy J F.1963. The mechanics of dunes and antidunes in erodible-bed channels. Journal of Fluid Mechanics, 16(4): 521-544.
[39] Kennedy J F.1969. The formation of sediment ripples,dunes and antidunes. Annual Review of Fluid Mechanics, 1(1): 147-168.
[40] Koloseus H J,Davidian J.1966. Free-surface instability correlations,and roughness-concentration effects on flow over hydrodynamically rough surfaces. Water Supply Paper,1592-C:1-72.
[41] Langford R,Bracken B.1987. Medano Creek,Colorado,a model for upper-flow-regime fluvial deposition. Journal of Sedimentary Petrology, 57(5): 863-870.
[42] Latrubesse E M,Stevaux J C,Sinha R.2005. Tropical rivers. Geomorphology, 70(3): 187-206.
[43] Leeder M R.1983. On the interactions between turbulent flow,sediment transport and bedform mechanics in channelized flows. In: Modern and Ancient Fluvial Systems. Collinson J D, Lewin J (eds.). International Association of Sedimentology Special Publication, 6: 5-18.
[44] Mader N K,Redfern J.2011. A sedimentological model for the continental Upper Triassic Tadrart Ouadou Sandstone Member: Recording an interplay of climate and tectonics(Argana Valley;South-west Morocco). Sedimentology, 58(5): 1247-1282.
[45] McLoughlin S.1993. Plant fossil distributions in some Australian Permian non-marine sediments. Sedimentary Geology, 85: 601-619.
[46] Middleton G V.1965. Antidune cross-bedding in a large flume. Journal of Sedimentary Research, 35(4): 922-927.
[47] Middleton G V,Southard J B.1984. Mechanics of sediment movement. Society of Economic Paleontologists and Mineralogists Short Course, 3:401.
[48] Nichols G J,Fisher J A.2007. Processes,facies and architecture of fluvial distributary system deposits. Sedimentary Geology, 195(1): 75-90.
[49] North C P,Taylor K S.1996. Ephemeral-fluvial deposits: Integrated outcrop and simulation studies reveal complexity. AAPG Bulletin, 80(6): 811-830.
[50] Paola C,Wiele S M,Reinhart M A.1989. Upper regime parallel lamination as the result of turbulent sediment transport and low-amplitude bedforms. Sedimentology, 36(1): 47-59.
[51] Parker G.1996. Some speculations on the relation between channel morphology and channel-scale flow structures. In: Coherent Flow Structures in Open Channels. Ashworths P J,Bennett S J,Best J L,McLelland S J(eds). John Wiley & sons,New York: 423-458.
[52] Picard M D,High L R.1973. Sedimentary Structures of Ephemeral Streams. Developments in Sedimentology 17.Amsterdam: Elsevier, 223,1-32.
[53] Plink-Björklund P.2015. Morphodynamics of rivers strongly affected by monsoon precipitation: Review of depositional style and forcing factors. Sedimentary Geology, 323: 110-147.
[54] Plink-Björklund P,Birgenheier L.2013. Highly Seasonal Ancient Monsoonal River Systems: Depositional Style,Allogenic and Autogenic Controls. 10th International Conference on Fluvial Sedimentology,Leeds,206-207.
[55] Postma G, Kleverlaan K.2018. Supercritical flows and their control on the architecture and facies of small-radius sand-rich fan lobes. Sedimentary Geology, 364: 53-70.
[56] Røe S L.1987. Cross-strata and bedforms of probable transitional dune to upper-stage plane-bed origin from a Late Precambrian fluvial sandstone,northern Norway. Sedimentology, 34(1): 89-101.
[57] Røe S L,Hermansen M.1993. Processes and products of large,Late Precambrian sandy rivers in northern Norway. In: Alluvial Sedimentation. Marzo M,Puigdefabregas C. Blackwell,Oxford(eds). International Association of Sedimentology Special Publication, 17: 151-166.
[58] Shukla U K,Singh I B,Sharma M,Sharma S.2001. A model of alluvial megafan sedimentation: Ganga megafan. Sedimentary Geology, 144(3-4): 243-262.
[59] Sinha R,Friend P F.1994. River systems and their sediment influx,Indo-Gangetic plains,Northern Bihar,India. Sedimentology, 41(4): 825-845.
[60] Southard J B,Boguchwal L A.1990. Bed configurations in steady unidirectional flows: Part 2. Synthesis of flume data. Journal of Sedimentary Petrology, 60(5): 658-679.
[61] Spinewine B,Sequeiros O E,Garcia M H,Beaubouef R T,Sun T,Svoye B Parker G.2009. Experiments on wedge-shaped deep sea sedimentary deposits in minibasins and/or on channel levees emplaced by turbidity currents. Part Ⅱ. Morphodynamic evolution of the wedge and of the associated bedforms. Journal of Sedimentary Research, 79(8): 608-628.
[62] Syvitski J P M,Brakenridge G R.2013. Causation and avoidance of catastrophic flooding along the Indus River,Pakistan. GSA Today, 23(1): 4-10.
[63] Syvitski J P M,Cohen S,Kettner A J,Brakenridge G R.2014. How important and different are tropical rivers?An overview. Geomorphology, 227: 5-17.
[64] Ventra D,Cartigny M J B,Bijkerk J F,Acikalin S.2015. Supercritical-flow structures on a Late Carboniferous delta front: Sedimentologic and paleoclimatic significance. Geology, 43(8): 731-734.
[65] Wang B,Ding Q.2008. Global monsoon: Dominant mode of annual variation in the tropics. Dynamics of Atmospheres and Oceans, 44(3): 165-183.
[66] Yagishita K.1992. Recent studies on some sedimentary structures formed under upper-flow-regime conditions: Review and discussion. Annual Report of the Faculty of Education University of Iwate, 52: 85-95.
[67] Yu X H,Li S L,Chen B T, Tan C P, Xie J, Hu X N.2012. Interaction between downslope and alongslope processes on the margins of Daihai Lake,North China: Implication for deltaic sedimentation models of lacustrine rift basin. Acta Geologica Sinica, 86(4): 932-948.
[68] Yu X H,Li S L,Tan C P,Xie J,Chen B T,Yang F.2013. The response of deltaic systems to climatic and hydrological changes in Daihai Lake rift basin,Inner Mongolia,northern China. Journal of Palaeogeography, 2(1): 41-55.

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季节性河流体系高流态沉积构造特征:以内蒙古岱海湖半滩子河为例*

Sedimentary structures formed under upper-flow-regime in seasonal river system: A case study of Bantanzi River,Daihai Lake, Inner Mongolia

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季节性河流体系高流态沉积构造特征:以内蒙古岱海湖半滩子河为例^*