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当今沉积学研究热点讨论——第20届国际沉积学大会评述
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  • 英文篇名:Current Hot Topics of Sedimentology:Comment on the 20~(th) International Sedimentological Congress
  • 作者:朱筱敏 ; 谈明轩 ; 董艳蕾 ; 李维 ; 秦祎 ; 张自力
  • 英文作者:ZHU XiaoMin;TAN MingXuan;DONG YanLei;LI Wei;QIN Yi;ZHANG ZiLi;College of Geosciences,China University of Petroleum (Beijing);Research Institute of Exploration and Development,SINOPEC Jiangsu Oilfield Company;
  • 关键词:国际沉积学大会 ; 研究热点 ; 人类世沉积 ; 湖泊沉积环境 ; 沉积过程 ; 深水重力流 ; “源—汇”系统 ; 微生物岩 ; 发展趋势
  • 英文关键词:International Sedimentological Congress;;hot topics;;anthropocene sedimentology;;lacustrine sedimentary system;;sedimentary process;;deep gravity flow;;"source-to-sink" system;;microbialites;;development trend
  • 中文刊名:CJXB
  • 英文刊名:Acta Sedimentologica Sinica
  • 机构:中国石油大学(北京)地球科学学院;中国石化江苏油田分公司勘探开发研究院;
  • 出版日期:2019-02-10
  • 出版单位:沉积学报
  • 年:2019
  • 期:v.37
  • 基金:国家自然科学基金项目(41072164)~~
  • 语种:中文;
  • 页:CJXB201901001
  • 页数:16
  • CN:01
  • ISSN:62-1038/P
  • 分类号:4-19
摘要
第20届国际沉积学大会于2018年8月13日—17日在加拿大魁北克城召开。来自51个国家、930余名专家学者参加了本次会议。基于本届大会论文专题设置情况,指出目前沉积学研究热点主要包含人类世沉积学、湖泊沉积环境、深水沉积过程、"源—汇"系统、微生物岩沉积学及沉积过程模拟等多个主要方面。当前人类活动对地貌影响、沉积物收支平衡影响不容忽视;湖泊沉积砂体研究不仅具有油气勘探价值,而且对古气候研究具有重要意义;沉积深水重力流的流态特征、沉积机理及实地监测等研究取得较大进展;"源—汇"系统研究思想在盆地构造演化、源区母岩性质及沉积物分散样式等方面具有更加实际的指导意义;微生物岩沉积学研究进展包括微生物矿化作用、成岩作用及其对于古地理重建的意义等方面;沉积物风化过程及其在不同环境下搬运及沉积过程是目前沉积学物理、数值模拟的主要内容。就近年来国际沉积学会议热点以及国际重点地质研究计划的实施情况来看,认为深时沉积记录、过程—产物研究方法、多学科交叉渗透是未来若干年内沉积学的发展方向。我国当今沉积学研究以应用沉积学为主,除了重视现代实验分析技术,还应加强野外基本地质研究方法和沉积过程机理研究。在沉积学快速发展的黄金时期,应抓住难得的机遇,不断将我国沉积学研究推向国际先进水平。
        The 20~(th) International Sedimentological Congress was held in Quebec City( Canada) from August 13~(th) to 17~(th) in 2018. 931 scholars from 51 countries attended this conference. According to the arrangement of sessions in the conference,the current hot topics contain Anthropocene sedimentology,lacustrine sedimentology,deep-water sedimentary process,"source-to-sink"system,microbialites and the simulation of sedimentary process et al. The anthropic influence on modern geomorphological characteristics cannot be unneglected. The study of lacustrine sandbodies is not only meaningful for petroleum exploration and development but also has great implications for paleoclimate. Flow characteristics,sedimentary process and situ monitoring of deep-water sediment gravity flows have made great achievements in recent years. "Source-to-sink"perspectives are instructive to tectonic evolution of sedimentary basin,the nature of parent rocks from provenance area and the sedimentary dispersal characteristics. The recent advancement of microbialites mainly consists of mineralization and diagenesis of microorganisms and their implications for the reconstruction of paleoclimate. The weathering of sedimentary rocks as well as subsequent transportation and sedimentation in different depositional environments have become the main research focus of physical and numerical simulation. According to hot topics of recent meetings of sedimentology and the implementation of major geological plans,deep-time depositional record,process-product study,multidisciplinary investigation will be development directions of sedimentary research in the following years. Current sedimentary research in our country still concentrates on applied sedimentology,we not only pay much attention to modern experimental and testing technology,but also to fundamental field work and mechanism of sedimentary process. During the golden age of the fast development of sedimentology,youth sedimentologists should not miss this rare opportunity to grow into the tower of strength of domestic sedimentology,and reach the word-class level as soon as possible in the future.
引文
[1]朱筱敏,李顺利,潘荣,等.沉积学研究热点与进展:第32届国际沉积学会议综述[J].古地理学报,2016,18(5):699-716.[Zhu Xiaomin,Li Shunli,Pan Rong,et al. Current hot topics and advances of sedimentology:A summary from 32nd IAS Meeting of Sedimentology[J]. Journal of Palaeogeography,2016,18(5):699-716.]
    [2] Crutzen P J,Stoermer E F. The “Anthropocene”[J]. Global Change Newsletter,2000,41:17-18.
    [3] Smith B D,Zeder M A. The onset of the Anthropocene[J]. Anthropocene,2013,4:8-13.
    [4] Syvitski J P M. The anthropocene—from concept,to geological epoch,to 21st century science[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City:IAS,2018.
    [5] Gibling M R. When did humans start to influence rivers?[C]//Proceedings of the 20th International Sedimentological Congress.Quebec City,2018.
    [6] Vorosmarty C J,Meybeck M,Fekete B,et al. The potential impact of neo-Castorization on sediment transport by the global network of rivers[M]//Walling D E,Probst J L. Human impact on erosion and sedimentation. Wallingford:IAHS Publication,1997:261-273.
    [7] Syvitski J P M,Kettner A J,Overeem I,et al. Anthropocene metamorphosis of the Indus Delta and lower floodplain[J]. Anthropocene,2013,3:24-35.
    [8] Syvitski J P M,Saito Y. Morphodynamics of deltas under the influence of humans[J]. Global and Planetary Change,2007,57(3/4):261-282.
    [9] Johwa G,Geris J,Comte J C,et al. Characterization of recent sediments from the Notwane Dam(Bostswana):preliminary results from the pula project[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [10] Waters C N,Zalasiewicz J,Summerhayes C,et al. The Anthropocene is functionally and stratigraphically distinct from the Holocene[J]. Science,2016,351(6269):aad2622.
    [11] Makri S,Martin G,Rey F,et al. Long-term high resolution records of productivity and meromixis from lake sediments using hyperspectral imaging spectroscopy:methods and applications[C]//Proceedings of the 20th International Sedimentological Congress.Quebec City,2018.
    [12] Zalasiewicz J,Waters C N,do Sul J A I,et al. The geological cycle of plastics and their use as a stratigraphic indicator of the Anthropocene[J]. Anthropocene,2016,13:4-17.
    [13] Pleskot K,Pelechata A,Pelechaty M,et al. Recent varve sedimentation in a lake under strong anthropogenic pressure. A case study of Lake Kierskie,western Poland[C]//Proceedings of the20th International Sedimentological Congress. Quebec City,2018.
    [14] Bristow C S,Holmes J. Sedimentology of the Holocene Angamma delta,Bodele depression,paleolake mega-chad[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [15] Xu Z,Wu S. Architecture and depositional process of bird-foot shoal-water delta:insights from modern deposits in Poyang Lake,China[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [16] Huang L,Pan J,Tang Y. From alluvial fan to gentle-slope conglomerate fan delta of shallow water,a new understanding of sedimentary promoted the new discovery in Mahu Slope Area of Xinjiang Junggar Basin[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [17] Wang J,Jiang Z,Xian B. A method to define the palaeowind strength from lacustrine beach ridge thickness[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [18] Su N,Fan S. Sedimentary characteristics and formation mechanism of thick layer lacustrine beach-bars in the Cenozoic basin of eastern China[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [19] Zhang T,Bai B,Wu Y,et al. Original types,microfacies and migration trajectory of sand beach-bar in interior depression lacustrine basins-Case study of Lower Jurassic,Central Sichuan Basin and Upper Triassic,Ordos Basin[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [20] Li X,Liu H,Pan S. The past,present and future of research on deep-water sedimentary gravity flow in lake basin of China[C]//Proceedings of the 20th International Sedimentological Congress.Quebec City,2018.
    [21] Scholz C A. Gravity flow deposits in large rift lakes:a case study of the Central Basin of the Lake Malawi(Nyasa)Rift[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [22] Pan S,Liu H,Liu C. Sublacustrine hyperpycnal channel-fan complex in the Songliao Basin,Northeast China[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [23] Li J,Chen G,Xie M,et al. The discovery of hyperpycnal flow in nonmarine rifted basin:a case study in Hailar Basin,China[C]//Proceedings of the 20th International Sedimentological Congress.Quebec City,2018.
    [24] Yang R,van Loon A J,Fan A,et al. The significance of finegrained gravity-flow deposits in the Late Triassic Yanchang Formation(Ordos Basin)for unconventional petroleum exploration[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [25] Parker G. Some speculations on the relation between channel morphology and channel-scale flow structures[M]//Ashworth P,Bennet S J,Best J L,et al. Coherent flow structures in open channels.New York:John Wiley&Sons,Inc.,1996:429-432.
    [26]谈明轩,朱筱敏,刘伟,等.旋回阶梯底形的动力地貌及其相关沉积物发育特征[J].地质论评,2017,63(6):1512-1522.[Tan Mingxuan,Zhu Xiaomin,Liu Wei,et al. The Morphodynamics of cyclic steps and sedimentary characteristics of associated deposits[J]. Geological Review,2017,63(6):1512-1522.]
    [27] Slootman A,Cartigny M J. A new classification of cyclic steps and its application[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [28] Peakall J,Best J,Baas J,et al. An integrated process-based model of flutes and tools in deep-marine systems[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [29] Yin D W,Peakall J,Parsons D,et al. Bedform genesis in bedrock substrates:insights into formative processes from a new experimental approach and the importance of suspension-dominated abrasion[J]. Geomorphology,2016,255:26-38.
    [30] Hage S,Cartigny M J B,Clare M A,et al. How to recognize crescentic bedforms formed by supercritical turbidity currents in the geologic record:Insights from active submarine channels[J]. Geology,2018,46(6):563-566.
    [31] Cartigny M J B,Eggenhuisen J T,Hansen E W M,et al. Concentration-dependent flow stratification in experimental high-density turbidity currents and their relevance to turbidite facies models[J].Journal of Sedimentary Research,2013,83(12):1047-1065.
    [32] Zavala C. Types of hyperpycnal flows and deposits in lacustrine and marine basins[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [33] Azpiroz-Zabala M,Cartigny M J B,Talling P J,et al. Newly recognized turbidity current structure can explain prolonged flushing of submarine canyons[J]. Science Advances, 2017, 3(10):e1700200.
    [34] Cartigny M J. How new deep-sea observations change turbidity current models[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [35] Clarke J E H. First wide-angle view of channelized turbidity currents links migrating cyclic steps to flow characteristics[J]. Nature Communications,2016,7:11896.
    [36] Liu Z,Zhao Y,Zhang Y,et al. Suspended sediment transport processes in the South China Sea:in-situ mooring observation process[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [37] Hodgson D M,Bernhardt A,Clare M A,et al. Grand challenges(and great opportunities)in sedimentology,stratigraphy,and diagenesis research[J]. Frontiers in Earth Science,2018,6:173
    [38] Gough A,Hall R,Mc Neil J. Sediment provenance and routing pathways in the Salin sub-basin,Myanmar[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [39] Aitchison J,Milan L,Murphy R. What did India collide with in the Early Eocene? Characterizing the sediment source of the Chulung La Formation,Ladakh,NW India[C]//Proceedings of the20th International Sedimentological Congress. Quebec City:IAS,2018.
    [40] Dew R E C,Collins A S,King R,et al. A detrital provenance story from Gondwana to northwest Thailand[C]//Proceedings of the20th International Sedimentological Congress. Quebec City,2018.
    [41] Robin C,Ponte J P,Guillocheau F,et al. The Zambezi Offshore system(delta to deep-sea fan):sink measurement-A record of the East African Riftu uplift and related climate changes[C]//Proceedings of the 20th International Sedimentological Congress.Quebec City,2018.
    [42] Guillocheau F,Robin C,Baby G,et al. Source to sink study at continent-scale(Africa):mantle dynamics controls and implications for the sediment routing system[C]//Proceedings of International Meeting of Sedimentology 2017. Toulouse,2017.
    [43] Li S,Cheng C,Chai G. The stratigraphy ages of the weakly metamorphic rocks in south Anhui and constraint on the tectonic evolution of the Jiangnan Orogenic Belt,South China[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [44] Liebermann C,Gough A,Hall R,et al. Provenance of sediments from Sumatra,Indonesia. Insights from detrital U-Pb ages,light and heavy minerals supported by Raman spectroscopy[C]//Proceedings of the 20th International Sedimentological Congress.Quebec City,2018.
    [45] Xu J,Snedden J,Stockli D,et al. Insights into the sediments sources and sand transport from onshore to abyssal plain from detrital zircon analyses of Gulf of Mexico Miocene deepwater fans[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [46] Ingersoll R V. Using autistic sand(stone)petrofacies to study the composition of modern sand and Cretaceous sandstone derived from the Sierra Nevada,California,USA,with implications for Cenozoic and Mesozoic uplift and dissection of a continental-margin magmatic arc[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [47] Chen H,Wood L,Gawthorpe R L. Linkage between margin delta systems and submarine fans in rifted basin-a example from Dampier sub-basin in offshore NW shelf of Australia[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [48] Liu H. Seismic geomorphology and architecture of early Miocene multi-sage shallow turbidite system,Yingggehai Basin,Northern South China Sea[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [49] Zhu X,Ge J,Zhang X,et al. Source to sink system of Wenchang formations in Lufeng Sag,Pearl Mouth Basin,China[C]//Proceedings of the 20th International Sedimentological Congress.Quebec City,2018.
    [50] Zhou X,Hou G,He M. Rock provenance and geomorphic controls on sand deposition in the large compressive basin-A case study of Huagang Formation in Xihu Depression,East China Sea Basin[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [51]戴永定,陈孟莪,王尧.微生物岩研究的发展与展望[J].地球科学进展,1996,11(2):209-215.[Dai Yongding,Chen Meng’e,Wang Yao. Development and perspective of research for microbolites[J]. Advance in Earth Sciences,1996,11(2):209-215.]
    [52] Burne R V,Moore L S. Microbialites:organosedimentary deposits of benthic microbial communities[J]. Palaios,1987,2(3):241-254.
    [53] Baud A,Richoz S,Brandner R,et al. Sponge-microbial buildups:a new look at the enigmatic basal Triassic“crystal layers”of central Iran[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [54] You X. Primary microbial dolomite in the middle Cambrian sabkha environment in the Tarim Basin,NW China[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [55] Song J,Liu S,Luo P,et al. Characteristics of microbial carbonate reservoirs in Middle Triassic Leikoupo Formation(Anisian Stage),Sichuan Basin,China[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [56] Brasier A T,Dennis P F,Still J,et al. Microbial or not microbial?Laminated carbonate-siliciclastic domes in the Mesoproterozoic Stoer Group,Scotland,UK[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [57] Mc Neil M,Webster J,Beaman R J,et al. New data reveals the complexity of modern Halimeda algal bioherm morphology in the Great Barrier Reef,Australia[C]//Proceedings of International Sedimentological Congress. Quebec City:IAS,2018.
    [58] Zhai X,Jiang H,Luo P,et al. Microbial growth in carbonate buildup and reservoir-implications from upper Sinian Dengying Formation of Sichuan Basin[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [59] Ko2irv A,Pérez A. Growth mechanisms of needle fibre calcite:is microbial metabolism involved?[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [60] Visscher P T,Pace A,Bouton A,et al. Microbial mechanisms of mineral precipitation:old wine in new bottles[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [61] Bourillot R,Vennin E,Pace A,et al. Looking for environmentaland bio-signatures in hypersaline microbialites:a comparison of ancient and modern sedimentary systems[C]//Proceedings of the20th International Sedimentological Congress. Quebec City,2018.
    [62] Martignier A,Jaquet J M,Filella M,et al. Micropearls:a widespread biomineralization process[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [63] Foubert A,Jaramillo-Vogel D,Negga H,et al. Spatial and temporal heterogeneity of microbialites and aragonite crusts in the Danakil Depression(northern Afar,Ethiopia)[C]//Proceedings of the20th International Sedimentological Congress. Quebec City,2018.
    [64] Bibi S,Oualha M,Suleiman M T,et al. Isolation,identification and application of indigenous ureolytic bacteria in microbially induced calcite precipitation(MICP)for soil stabilization at harsh Conditions[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [65] Bougeault C,Durlet C,Vennin E,et al. A typical carbonate-silica mineralisations under biotic and abcontrols:the modern hydrothermal example of Pastos Grandes Laguna(Bolivia)[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [66] Barilaro F,Di Capuam A,Mc Kenzie J A,et al. Abiotic versus biotic control in hydrothermal travertine precipitation[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [67] Porta G D,Reitner J,Reimer A. The influence of microbial mats on travertine precipitation in active hydrothermal systems from central Italy[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [68] Al Disi Z,Bontognali T,Jaoua S,et al. The effect of temperature,salinity and Mg2+:Ca2+ratio on microbially-mediated Mg-rich car- bonates by aerobic isolated from a Sabkha environment[C]//Proceedings of the 20th International Sedimentological Congress.Quebec City,2018.
    [69] Roche A,Vennin E,Bouton A,et al. Effect of substrate on the microbialite development[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [70] Eymard I,Alvarez M P,Bilmes A,et al. Fossil and living freshwater microbialites in Northeastern Patagonia(Argentina)[C]//Proceedings of the 20th International Sedimentological Congress.Quebec City,2018.
    [71] Danisch J,Nutz A,Kabiri L,et al. The evolution of carbonate factories in the late Sinemurian-Pliensbachian transition-case study from the high Atlas Mountains(Morocco)[C]//Proceedings of the20th International Sedimentological Congress. Quebec City,2018.
    [72] Wen H,Xu W,Wen L,et al. Genetic mechanisms of oncoids in the Givetian(Middle Devonian)Jinbaoshi Formation of the Longmenshan area,Sichuan,China[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [73] Bai Y,Luo P,Liu W. Storm deposits and accompanying microbial bioherms in Sugaitblak and Yutixi area,NW Tarim Basin,China[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [74] Bourillot R,Vennin E,Pace A,et al. Looking for environmentaland bio-signatures in hypersaline microbialites:a comparison of ancient and modern sedimentary systems[C]//Proceedings of the20th International Sedimentological Congress. Quebec City,2018.
    [75] Bouton A,Vennin E,Pace A,et al. Microbialites preserved the sedimentary record:are they an accurate view of the microbial activity?[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [76] Bourillot R,Vennin E,Pace A,et al. Looking for environmentaland bio-signatures in hypersaline microbialites:a comparison of ancient and modern sedimentary systems[C]//Proceedings of the20th International Sedimentological Congress. Quebec City,2018.
    [77] Gerson J,Terra S. Marine X Continental deposits-lessons from unexpected environments like pre-salt carbonates in Brazil[C]//Proceedings of the 20th International Sedimentological Congress.Quebec City,2018.
    [78] Riding R,Virgone A. Hybrid carbonates:abiotic-microbial-skeletal[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [79] Peryt T M,Raczyński P,Jasionowski M,et al. Transition from bryozoan-to microbial-dominant reefs in the Zechstein limestone(Lopingian)of west Poland[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City:IAS,2018.
    [80] Desrochers A,Zhan R,Luan X,et al. Oolitic and microbial limestones as time-specific facies in the aftermath of the End-Ordovician mass extinction and glaciation[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [81] Lee J,Dattilo B F,Mrozek S,et al. Lithistid sponge-microbial reefs,Nevada,USA:filling the late Cambrian:’reef gap’[C]//Proceedings of the 20th International Sedimentological Congress.Quebec City,2018.
    [82] Yao L,Aretz M,Chen J,et al. Denayer Global microbial carbonate proliferation after the End-Devonian mass extinction and a comparison to other major extinctions[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [83] Stagner A,James N,Zulian M,et al. Frasnian Pinnacle Reefs,western Canadian sedimentary basin:a product of environmental not evolutionary change[C]//Proceedings of the 20th International Sedimentological Congress. Québec City,2018.
    [84] Husinec A. Microbial carbonates as recorders of sea-level,accommodation space,and salinity changes:upper Ordovician Williston Basin,North Dakota[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City:IAS,2018.
    [85] Ji Y,Zhou Y,Zhou Y,et al. Sedimentary characteristics and sedimentary model of interbedded carbonate and clastic rocks in the Paleogene lacustrine basin,western Qaidam Basin,China[C]//Proceedings of the 20th International Sedimentological Congress.Quebec City,2018.
    [86] Bai Y,Luo P,Liu W. Sedimentary characteristics of microbial carbonate and its response to sequence stratigraphic framework:implication for the lower Cambrian Xiaoerblak Formation,NW Tarim Basin[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [87] Chen D,Song Y,Guo C,et al. Early Cambrian dolomite microbial buildups in the Tarim Basin(NW China)[C]//Proceedings of the20th International Sedimentological Congress. Quebec City,2018.
    [88] Wen Y,Wang C,Gao Y,et al. Facilitation of microbial metabolism on the nucleation and diagenetic stabilization of Eocene dolomite from the Lunpola Basin,central Tibet[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [89]曹耀华,赖志云,刘怀波,等.沉积模拟实验的历史现状及发展趋势[J].沉积学报,1990,8(1):143-147.[Cao Yaohua,Lai Zhiyun,Liu Huaibo,et al. Sedimentary simulation experiments:in the past,current states,and developing trend[J]. Acta Sedimentologica Sinica,1990,8(1):143-147.]
    [90]朱筱敏,钟大康,袁选俊,等.中国含油气盆地沉积地质学进展[J].石油勘探与开发,2016,43(5):820-829.[Zhu Xiaomin,Zhong Dakang,Yuan Xuanjun,et al. Development of sedimentary geology of petroliferous basins in China[J]. Petroleum Exploration and Development,2016,43(5):820-829.]
    [91] Paredis B,Weltje G J. Numerical modeling of sediment generation:characterization of parent rock properties[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [92] Zhou X,Hou G,He M. Simulating large-scale sand deposit in the mixed fluvial system-a case study of Huagang formation in Xihu Depression,East China Sea Basin[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [93] Rieux A,Weill P,MouazéD,et al. Sorting processes and internal architecture of bio-siliciclastic coastal barriers:physical modelling[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City:IAS,2018.
    [94] Wang Y,Abels H A,Joep E,et al. Modelling orbital climate signals in fluvial stratigraphy[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [95] Lin Z,Wang C,Shan J,et al. Three-dimensional distribution characteristics of migration architecture elements of meandering rivers based on slice simulation experiment[C]//Proceedings of the20th International Sedimentological Congress. Quebec City,2018.
    [96] Zhou H,Yin Y,Huang J,et al. Influence factors on the distribution of tidal bar in tide-dominated estuary:insight from deposition numerical simulation[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [97] Paumard V,Bourget J. Accomodation,sediment supply,deltaic regime and their controls on sand delivery to deep water:insights from quantitative 3D seismic stratigraphy(QQS)[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [98] Wang H,Wang Z,Ye L. The couplinf relationship between shelfmargin delta and deep water deposit[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [99] Feng W,Zhang C,Yin Y,et al. Fan delta controlled by autogenic process:implications from a flume-tank experiment[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.
    [100] Chen J,Li Q,Zhu R,et al. Physical simulation and mechanism of soft-sediment slump deformation[C]//Proceedings of the 20th International Sedimentological Congress. Quebec City,2018.

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