沉积学研究热点与进展:第19届国际沉积学大会综述
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摘要
基于第19届国际沉积学大会资料,分析了当前国际沉积学研究热点和研究进展,指出除了资源沉积学研究持续走热外,全球气候变化沉积记录、深水沉积与事件沉积和碳酸盐与微生物沉积成为当前沉积学3大热门研究领域。全球气候沉积记录领域的进展表现在气候的沉积记录载体研究,特殊地质时期或地域气候效应及早期气候宏观变化规律研究;深水沉积与事件沉积领域的进展包括水力跳跃、深水实地监测等重力流沉积过程研究,地震、海啸、洪水、火山等事件沉积学及重力流沉积预测及油气勘探;碳酸盐与微生物沉积领域的进展包含冷水碳酸盐沉积和微生物对碳酸盐沉积的控制。对比表明,中国沉积学研究在环境上关注河湖等陆相多,风成、冰川和海岸等研究较薄弱;性质上以资源沉积学等应用研究为主导,沉积动力过程等基础研究薄弱;热点领域上对深水沉积和非常规油气领域关注多,但多局限于沉积现象描述与油气勘探开发实践。笔者指出,注重碎屑物沉积动力过程和源—渠—汇系统分析,及时引进深水和冷水碳酸盐沉积理论、发展生物地质学,充分利用大量科探和油田钻孔资料开展全球气候研究,是近期中国沉积学突破的可能方向。
The current research hotspots and advances of international sedimentology has been analyzed based on the data of 19 th International Sedimentological Congress,which indicates that global climatic sedimentary record,deepwater sedimentology and event deposition,and carbonate and microbialsedimentology are becoming the three current hot issues in sedimentology besides the continual hot topic:resources sedimentology. Main progresses in global climate sedimentary record came from sedimentary recorders exploration for detailed climate change,climatic environmental and ecological effects and the climate macro-change rules of deep time in a special geological time or a special geological realm. Main advances in deepwater sedimentology and event deposition were embodied in sedimentary process study,such as hydraulic jump and field monitoring of deepwater sedimentary process,and event deposition triggered by earthquake,tsunami,flood,volcanic,etc.,and the turbidite prediction and hydrocarbon exploration. Advances in carbonate and microbial sedimentology were expressed in cold water carbonate deposition and microbial controls on carbonate deposition. Comparison shows that sedimentary study in China focuses on continental facies such as fluvial and lacustrine but seldom on eolian,glacier and coastal environment; focuses on applied resource sedimentology and so forth,but rarely on basic scientific problems such as sedimentary dynamic process study in terms of the study objectives; focuses more on deepwater sedimentation and unconventional resource geology in three hot issues,but confined them to the sedimentary phenomenon description,hydrocarbon exploration and development. Finally,the authors suggest that three breakthrough directions possibly come from more attentions paid to sedimentary dynamic process and source-channel-sink system analysis,and timely introduction of the deepwater and cold carbonate sedimentation and biological geology theory,and global climate change studies with full-use of a large number of scientific drillings and wells information from oilfield drilling.
The current research hotspots and advances of international sedimentology has been analyzed based on the data of 19 th International Sedimentological Congress,which indicates that global climatic sedimentary record,deepwater sedimentology and event deposition,and carbonate and microbialsedimentology are becoming the three current hot issues in sedimentology besides the continual hot topic:resources sedimentology. Main progresses in global climate sedimentary record came from sedimentary recorders exploration for detailed climate change,climatic environmental and ecological effects and the climate macro-change rules of deep time in a special geological time or a special geological realm. Main advances in deepwater sedimentology and event deposition were embodied in sedimentary process study,such as hydraulic jump and field monitoring of deepwater sedimentary process,and event deposition triggered by earthquake,tsunami,flood,volcanic,etc.,and the turbidite prediction and hydrocarbon exploration. Advances in carbonate and microbial sedimentology were expressed in cold water carbonate deposition and microbial controls on carbonate deposition. Comparison shows that sedimentary study in China focuses on continental facies such as fluvial and lacustrine but seldom on eolian,glacier and coastal environment; focuses on applied resource sedimentology and so forth,but rarely on basic scientific problems such as sedimentary dynamic process study in terms of the study objectives; focuses more on deepwater sedimentation and unconventional resource geology in three hot issues,but confined them to the sedimentary phenomenon description,hydrocarbon exploration and development. Finally,the authors suggest that three breakthrough directions possibly come from more attentions paid to sedimentary dynamic process and source-channel-sink system analysis,and timely introduction of the deepwater and cold carbonate sedimentation and biological geology theory,and global climate change studies with full-use of a large number of scientific drillings and wells information from oilfield drilling.
引文
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汉景泰.2013.黄土[A].见:冯增昭.中国沉积学(第二版)[M].北京:石油工业出版社,482-506.
吴因业,朱如凯,罗平,等.2011.沉积学与层序地层学研究新进展:第18届国际沉积学大会综述[J].沉积学报,29(1):199-206.
Aurell M,Bdenas B.2014.Sedimentary Evolution of a Microbial-siliceous Sponge Dominated Carbonate Platform(Bajocian,Iberian Basin,Spain)[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,32.
Banerjee S.2014.Microbial Mat-related Structures in Siliciclastics asPalaeo-environmental Proxies:Examples from Precambrian Vindhyan Basin and Modern Gulf of Cambay,India[A].In:Abstracts Bookof 19th International Sedimentological Congress[C].Geneva:University of Geneva,42.
Brandano M,Cuffaro M,Gaglianone G,et al.2014.Quantifying theContribution of Seagrass Carbonate Factories from the Paleocene tothe Present[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,95.
Cao Y,Yang T,Wang Y,et al.2014.Classification of Subaqueous Sedimentary Gravity Flows and Recognition of Their Deposit in Lacustrine Basin with Example of Jiyang Depression,East China[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,118.
Cartigny M J B,Watkins H,Vellinga A J,et al.2014.What can Supercritical-flow Bedforms Tell Us About the Internal Structure of Turbidity Currents?[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,120.
Cazenave A.2014.Sea Level Rise:Recent Past,Present and Future[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,4.
Chen X,Wang C,Wu H,et al.2014.Orbitally Forced Sea Level Changes in the Cemanian of the Tethyan Himalaya[A].In:AbstractsBook of 19th International Sedimentological Congress[C].Geneva:University of Geneva,141.
Ciurej A,Haczewski G.2014.Diagenetic Overprint on the Primary Record in Varved Coccolith Limestones,Lower Oligocene,Outer Carpathians[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,153.
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De Gasperi A,Catuneanu O.2014.Sequence stratigraphy of the EoceneTurbidite Reservoirs in Albacora Field,Campos Basin,Offshore Brazil[J].AAPG Bulletin,98(2):279-313.
Droeven C,Pacton M,Bahniuk,et al.2014.Impact of Microbial Activityon Reservoir Quality in Tuffaceous Sediments[A].In:AbstractsBook of 19th International Sedimentological Congress[C].Geneva:University of Geneva,189.
Escutia C.2014.Sedimentary Records of the Ice Sheet Behavior DuringPast Warm Intervals:An Ocean Drilling Strategy[A].In:AbstractsBook of 19th International Sedimentological Congress[C].Geneva:University of Geneva,1.
Feenstra E J,Vonhof H B,Mienis F,et al.2014.Stable Isotopes of Fluid Inclusions:A New Method to Ground Truth Climate Archives inCoral Skeletons[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,207.
Goldfinger C,Patton J R,Morey A E,et al.2014.Third Generation Paleoseismology:Convolving Sedimentology with Site Analysis,SlopeStability and the Earthquake Source in Sub-aqueous Settings[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,248.
Guo H,Du Y S,Kah L C,et al.2014.Biological Activity and theEarth's Surface Evolution in Early Mesoproterozoic:Insights fromCarbon and Sulfur Isotope Records of the Jixian Group,North China[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,270.
Haughton P D W,Barker S P,Mc Caffrey W D.2003.‘Linked'debritesin sand-rich turbidite systems:Origin and significance[J].Sedimentology,50(3):459-482.
Hong S K,Shinn Y J.2014.Early Cretaceous Atmospheric Carbon Dioxide Concentration Estimated from Pedogenic Carbonates in the Gyeongsang Basin,Korea[A].In:Abstracts Book of 19th InternationalSedimentological Congress[C].Geneva:University of Geneva,296.
Hu X M,Zhao K D,Li Y X,et al.2014.Paleoceanographic Transitionfrom the Aptian Oceanic Anoxic Event 1a(Oae1a)to the OceanicRed Bed 1(Orb1)in the Gorgo a Cebara Section(Central Italy)[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,302.
Hubbard S M,Romans B W,Jobe Z R,et al.2014.Measuring the Number of Turbidity Currents that Pass Through Submarine Channels[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,302.
James N P.2014.Unlikely Carbonates:They Are So Cool![A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,5.
Kettler R M,Loope D B W,Karrie A,et al.2014.Microbially MediatedIron-Oxide Bands at Petra(southern Jordan)Are Oxidation Productsof Late Diagenetic Siderite[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,348.
Leu M,Baud A,Brosse M,et al.2014.Earthquake Induced Soft Sediment Deformation(seismites):New Data from the Early Triassic Guryul Ravine Section(Kashmir)[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University ofGeneva,396.
Li X,Chen Q,Liu H,et al.2014.Argillaceous Parcel:A Criterion forRecognizing Sandy Mass-Transport Deposits:Deep-water MassiveSandstone of the Yanchang Formation(Upper Triassic),Ordos Basin,Central China[A].In:Abstracts Book of 19th InternationalSedimentological Congress[C].Geneva:University of Geneva,410.
Liu H,Chen Q,Li X,et al.2014.Sedimentary Characteristics and Seismic Geomorphology of Gravity-flow Channels in Rifted Basin:Oligocene Shahejie Formation,Qinan Slope,Huanghua Depression of Bohai Bay Basin,China[A].In:Abstracts Book of 19th InternationalSedimentological Congress[C].Geneva:University of Geneva,432.
Malgesini G,Talling P J,Armitage D,et al.2014.Quantitative Analysisof Submarine-Flow Deposit Shape in the Marnoso-Arenacea Formation[A].In:Abstracts Book of 19th International SedimentologicalCongress[C].Geneva:University of Geneva,462.
Martin-Puertas C,Tjallingii R,Deriot A,et al.2014.Evidence of RapidClimate Change at 10.77ka Coinciding with the Preboreal-BorealTransition in Central Europe:A Contribution from the Varved Record of Meerfelder Maar,Germany[A].In:Abstracts Book of 19thInternational Sedimentological Congress[C].Geneva:University ofGeneva,472.
Mattioli E,Salaviale C,Gollain B.2014.Impact of Pelagic CarbonateProduction(calcareous nannofossils)on CCD Fluctuations During theMiddle Eocene[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,476.
Merino-ToméO,Bahamonde J R,Della Porta G,et al.2014.The Palaeoequatorial Microbial Carbonate Province of the Cantabrian Zone(Pennsylvanian,NW Spain)[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,491.
Montanez I P.2014.Earth's Deep-Time Insight into Our Climate Future[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,2.
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Mulder T.2014.Flood record in marine sediments[A].In:AbstractsBook of 19th International Sedimentological Congress[C].Geneva:University of Geneva,6.
Polonia A,Cacchione D,Gasperini L.2014.Historic deep sea tsunamitesin the Ionian Sea[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,557.
Shanmugam G.1996.High-density turbidity currents:Are they sandydebris flows?[J].Journal of Sedimentary Research,66:2-10.
Shreeve J W,Talling P J,Wright I C,et al.2014.Origin of SpectacularSubmarine Bedform-like Morphologies Surrounding Volcanic Islands-Slope Failure or Eruption-Fed Bedforms?[A].In:Abstracts Bookof 19th International Sedimentological Congress[C].Geneva:University of Geneva,628.
Sowakiewicz M,Thomas L,Tucker M E,et al.2014.Biogeochemistry ofHolocene Intertidal Microbial Mats of Qatar:Implications for Petroleum Source Rock Formation in Carbonate-evaporite Systems[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,645.
Spezzaferri S,Stalder C,Rüggeberg A,et al.2014.Facies and BenthicForaminiferal Fauna from Cold-water Coral Mounds and Reefs:Toolsfor Paleoceanographic Reconstructions[A].In:Abstracts Book of19th International Sedimentological Congress[C].Geneva:University of Geneva,655.
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汉景泰.2013.黄土[A].见:冯增昭.中国沉积学(第二版)[M].北京:石油工业出版社,482-506.
吴因业,朱如凯,罗平,等.2011.沉积学与层序地层学研究新进展:第18届国际沉积学大会综述[J].沉积学报,29(1):199-206.
Aurell M,Bdenas B.2014.Sedimentary Evolution of a Microbial-siliceous Sponge Dominated Carbonate Platform(Bajocian,Iberian Basin,Spain)[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,32.
Banerjee S.2014.Microbial Mat-related Structures in Siliciclastics asPalaeo-environmental Proxies:Examples from Precambrian Vindhyan Basin and Modern Gulf of Cambay,India[A].In:Abstracts Bookof 19th International Sedimentological Congress[C].Geneva:University of Geneva,42.
Brandano M,Cuffaro M,Gaglianone G,et al.2014.Quantifying theContribution of Seagrass Carbonate Factories from the Paleocene tothe Present[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,95.
Cao Y,Yang T,Wang Y,et al.2014.Classification of Subaqueous Sedimentary Gravity Flows and Recognition of Their Deposit in Lacustrine Basin with Example of Jiyang Depression,East China[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,118.
Cartigny M J B,Watkins H,Vellinga A J,et al.2014.What can Supercritical-flow Bedforms Tell Us About the Internal Structure of Turbidity Currents?[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,120.
Cazenave A.2014.Sea Level Rise:Recent Past,Present and Future[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,4.
Chen X,Wang C,Wu H,et al.2014.Orbitally Forced Sea Level Changes in the Cemanian of the Tethyan Himalaya[A].In:AbstractsBook of 19th International Sedimentological Congress[C].Geneva:University of Geneva,141.
Ciurej A,Haczewski G.2014.Diagenetic Overprint on the Primary Record in Varved Coccolith Limestones,Lower Oligocene,Outer Carpathians[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,153.
Clare M,Talling P J,Hunt J E.2014.Extreme Global Warming and Submarine Landslide Activity:Cause and Effect at the Initial EoceneThermal Maximum and Implications for the Future[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,157.
De Gasperi A,Catuneanu O.2014.Sequence stratigraphy of the EoceneTurbidite Reservoirs in Albacora Field,Campos Basin,Offshore Brazil[J].AAPG Bulletin,98(2):279-313.
Droeven C,Pacton M,Bahniuk,et al.2014.Impact of Microbial Activityon Reservoir Quality in Tuffaceous Sediments[A].In:AbstractsBook of 19th International Sedimentological Congress[C].Geneva:University of Geneva,189.
Escutia C.2014.Sedimentary Records of the Ice Sheet Behavior DuringPast Warm Intervals:An Ocean Drilling Strategy[A].In:AbstractsBook of 19th International Sedimentological Congress[C].Geneva:University of Geneva,1.
Feenstra E J,Vonhof H B,Mienis F,et al.2014.Stable Isotopes of Fluid Inclusions:A New Method to Ground Truth Climate Archives inCoral Skeletons[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,207.
Goldfinger C,Patton J R,Morey A E,et al.2014.Third Generation Paleoseismology:Convolving Sedimentology with Site Analysis,SlopeStability and the Earthquake Source in Sub-aqueous Settings[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,248.
Guo H,Du Y S,Kah L C,et al.2014.Biological Activity and theEarth's Surface Evolution in Early Mesoproterozoic:Insights fromCarbon and Sulfur Isotope Records of the Jixian Group,North China[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,270.
Haughton P D W,Barker S P,Mc Caffrey W D.2003.‘Linked'debritesin sand-rich turbidite systems:Origin and significance[J].Sedimentology,50(3):459-482.
Hong S K,Shinn Y J.2014.Early Cretaceous Atmospheric Carbon Dioxide Concentration Estimated from Pedogenic Carbonates in the Gyeongsang Basin,Korea[A].In:Abstracts Book of 19th InternationalSedimentological Congress[C].Geneva:University of Geneva,296.
Hu X M,Zhao K D,Li Y X,et al.2014.Paleoceanographic Transitionfrom the Aptian Oceanic Anoxic Event 1a(Oae1a)to the OceanicRed Bed 1(Orb1)in the Gorgo a Cebara Section(Central Italy)[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,302.
Hubbard S M,Romans B W,Jobe Z R,et al.2014.Measuring the Number of Turbidity Currents that Pass Through Submarine Channels[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,302.
James N P.2014.Unlikely Carbonates:They Are So Cool![A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,5.
Kettler R M,Loope D B W,Karrie A,et al.2014.Microbially MediatedIron-Oxide Bands at Petra(southern Jordan)Are Oxidation Productsof Late Diagenetic Siderite[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,348.
Leu M,Baud A,Brosse M,et al.2014.Earthquake Induced Soft Sediment Deformation(seismites):New Data from the Early Triassic Guryul Ravine Section(Kashmir)[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University ofGeneva,396.
Li X,Chen Q,Liu H,et al.2014.Argillaceous Parcel:A Criterion forRecognizing Sandy Mass-Transport Deposits:Deep-water MassiveSandstone of the Yanchang Formation(Upper Triassic),Ordos Basin,Central China[A].In:Abstracts Book of 19th InternationalSedimentological Congress[C].Geneva:University of Geneva,410.
Liu H,Chen Q,Li X,et al.2014.Sedimentary Characteristics and Seismic Geomorphology of Gravity-flow Channels in Rifted Basin:Oligocene Shahejie Formation,Qinan Slope,Huanghua Depression of Bohai Bay Basin,China[A].In:Abstracts Book of 19th InternationalSedimentological Congress[C].Geneva:University of Geneva,432.
Malgesini G,Talling P J,Armitage D,et al.2014.Quantitative Analysisof Submarine-Flow Deposit Shape in the Marnoso-Arenacea Formation[A].In:Abstracts Book of 19th International SedimentologicalCongress[C].Geneva:University of Geneva,462.
Martin-Puertas C,Tjallingii R,Deriot A,et al.2014.Evidence of RapidClimate Change at 10.77ka Coinciding with the Preboreal-BorealTransition in Central Europe:A Contribution from the Varved Record of Meerfelder Maar,Germany[A].In:Abstracts Book of 19thInternational Sedimentological Congress[C].Geneva:University ofGeneva,472.
Mattioli E,Salaviale C,Gollain B.2014.Impact of Pelagic CarbonateProduction(calcareous nannofossils)on CCD Fluctuations During theMiddle Eocene[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,476.
Merino-ToméO,Bahamonde J R,Della Porta G,et al.2014.The Palaeoequatorial Microbial Carbonate Province of the Cantabrian Zone(Pennsylvanian,NW Spain)[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,491.
Montanez I P.2014.Earth's Deep-Time Insight into Our Climate Future[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,2.
Mulder T,Alexander J.2001.Abrupt change in slope causes variation inthe deposit thickness of concentrated particle-driven density currents[J].Marine Geology,175(1-4):221-235.
Mulder T.2014.Flood record in marine sediments[A].In:AbstractsBook of 19th International Sedimentological Congress[C].Geneva:University of Geneva,6.
Polonia A,Cacchione D,Gasperini L.2014.Historic deep sea tsunamitesin the Ionian Sea[A].In:Abstracts Book of 19th International Sedimentological Congress[C].Geneva:University of Geneva,557.
Shanmugam G.1996.High-density turbidity currents:Are they sandydebris flows?[J].Journal of Sedimentary Research,66:2-10.
Shreeve J W,Talling P J,Wright I C,et al.2014.Origin of SpectacularSubmarine Bedform-like Morphologies Surrounding Volcanic Islands-Slope Failure or Eruption-Fed Bedforms?[A].In:Abstracts Bookof 19th International Sedimentological Congress[C].Geneva:University of Geneva,628.
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