国际沉积学研究前沿和发展讨论——第37次国际沉积学家年会述评

doi:10.11743/ogg20250301

Abstract

Abstract:

The 37thInternational Meeting of Sedimentology （also referred to as the 37th IMS） was held in June 2024 in Aberdeen， UK， focusing on the frontiers of sedimentology. Specifically， this meeting highlighted cutting-edge academic issues including the interactions between the Earth， life， and climate， Precambrian environments， source-to-sink systems， fluvial and lacustrine sedimentation， tidal action and neritic sedimentation， deep-water sedimentation， and the diagenesis and reservoir characterization of siliceous clastic rocks. Additional focal areas included carbonate rocks and evaporites， ichnology， volcanoes and geochemistry， planetary sedimentology， geothermal resources and energy transition， seismic sedimentology， and AI-based new methodologies and technologies for sedimentological research. This meeting emphasized the importance of paleoclimate research in deciphering deep-time global changes， presenting a novel approach to reconstruct paleoclimate using high-resolution sedimentary records. It underscored the coupling relationships among tectonic activities， climate change， and sedimentary processes， positing that elucidating source-to-sink transport mechanisms necessitates multi-scale geomorphological reconstruction and sediment flux simulations. Furthermore， this meeting underlined the transport and deposition mechanisms of fine-grained sediments in deep-water environments， and introduced novel machine learning-based methods for automatic sedimentary facies identification， reservoir prediction， and sedimentary process simulation. A comprehensive analysis of the cutting edge obtained from the 37th IMS reveals that future sedimentological research in China should prioritize research on paleoclimate and deep-time global changes， paleogeomorphology and source-to-sink systems， deep-water sedimentation and fine-grained sedimentology， and new technologies such as big data and AI. The purpose is to achieve the national energy strategic objectives and establish a sedimentological theoretical system that reflects the regional geological characteristics of China.

Key words: big data and artificial intelligence （AI） technology, deep-time global climate, paleogeomorphology and source-to-sink system, deep-water sedimentation and fine-grained sedimentology, International Meeting of Sedimentology （IMS）

CLC Number:

TE121.3

Xiaomin ZHU, Xiaolin WANG, Xin HU, Xiang WANG, Zijie GAO. Frontiers and future prospects of international sedimentological research： Review on the 37th International Meeting of Sedimentology[J]. Oil & Gas Geology, 2025, 46(3): 685-704.

Figures/Tables 7

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93	LI G. Chemofacies characterization of lacustrine shale based on machine learning classification： A case study from the Dongying Depression， Bohai Bay Basin， China［C］//Abstract of the 37th International Meeting of Sedimentologists （IMS）， Aberdeen， UK， 2024.
94	HOUGHTON J. Quantifying porosity and permeability enhancing grain-coating clays in 3D using X-ray computed tomography （XCT）： An example from the Tilje Formation， Norwegian North Sea［C］//Abstract of the 37th International Meeting of Sedimentologists （IMS）， Aberdeen， UK， 2024.
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97	XU H. Terrigenous hot spring sinters and submarine hydrothermal smokers record changes of organic molecules： Implication for the search for biomolecules on Mars［C］//Abstract of the 37th International Meeting of Sedimentologists （IMS）， Aberdeen， UK， 2024.
98	ZHANG Kun. Effect of the hydrothermal activity in the Lower Yangtze region on marine shale gas enrichment： A case study of Lower Cambrian and Upper Ordovician-Lower Silurian shales in Jiangye-1 well［C］//Abstract of the 37th International Meeting of Sedimentologists （IMS）， Aberdeen， UK， 2024.
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100	ROBAN R D. Deciphering the early-stage evolution of relict marine basins： The case of the Ceahlău-Severin Ocean of the Romanian Carpathians［C］//Abstract of the 37th International Meeting of Sedimentologists （IMS）， Aberdeen， UK， 2024.
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序号	主题	代号	专题名称	序号	主题	代号	专题名称
1	碳酸盐岩	1.1	微生物碳酸盐岩沉积环境	9	地球、生命与气候	9.1	事件沉积记录
		1.2	白云石化作用			9.2	气候驱动沉积变化
		1.3	碳酸盐岩层序地层学			9.3	古环境演化
		1.4	碳酸盐岩岩相古地理			9.4	环境与生物群落
		1.5	碳酸盐岩储层评价			9.5	环境灾害沉积学
2	蒸发岩	2.1	蒸发岩古气候与沉积	10	碎屑岩成岩作用	10.1	人类活动对岩石圈影响
2	蒸发岩	2.2	蒸发岩同位素记录	10	碎屑岩成岩作用	10.2	成岩作用与孔隙发育
3	浅海碎屑岩	3.1	浅海沉积过程与沉积环境	11	储层表征	11.1	储层形成与评价
		3.2	古气候与古环境重建	11	储层表征	11.2	储层预测与流体识别
		3.3	浅水三角洲	12	地震沉积学	12.1	精细刻画及储层预测
4	潮汐作用	4.1	现代潮汐沉积作用	12	地震沉积学	12.2	薄储层地震成像
4	潮汐作用	4.2	地质历史的潮控三角洲	13	AI方法与技术	13.1	机器学习预测环境岩相及甜点
5	能源转型	5.1	CCUS			13.2	虚拟三维建模技术
5	能源转型	5.2	地热			13.3	沉积学数据库云平台构建
6	源-汇系统	6.1	物源分析	14	地热与火山	14.1	热液沉积与生物保存机制
6	源-汇系统	6.2	源-汇过程			14.2	古环境与火山作用
7	河流与湖泊	7.1	河流沉积与构造演化			14.3	火山沉积结构
		7.2	河流相储层勘探	15	深水沉积	15.1	水槽实验和现代浊流监测
		7.3	储层成因机制			15.2	混合事件层
		7.4	气候对河流沉积的影响			15.3	陆架到盆地的沉积物输送
8	遗迹化石	8.1	遗迹学与沉积环境	16	其他	16.1	科学钻探探索地球：IODP
8	遗迹化石	8.2	遗迹化石根源及保存	16	其他	16.2	其他沉积学专题

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Frontiers and future prospects of international sedimentological research： Review on the 37th International Meeting of Sedimentology

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