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多尺度的古地理学研究:思考与展望OA

Multi-scale palaeogeographic research:reflections and prospects

中文摘要英文摘要

地球表面的古地理单元呈现不同的级次,但其内涵、研究意义、重建尺度及方法的差异尚不明确,影响了古地理学的协调发展.古地理单元为具有一定气候、水文、生态特征的古地貌单元.依据地貌相对规模及其成因,将古地理单元分为大、中、小三级,相应地将古地理研究尺度分为三级.大尺度古地理研究为在全球及跨板块(盆地)的大区域内,以数百万年至数千万年为时间单元,研究大级次古地理单元(大洋、大陆及其内部的大型地貌起伏)的时空分布及多圈层相互作用,用于宜居地球及矿产资源远景区预测;中尺度古地理研究为在一个较大型地貌单元(如盆地)内,以数十万年为时间单元,研究中级次古地理单元(较大型地貌与亚环境之间的地貌单元)的特征、分布、变迁及相应的地表作用过程,用于人类宜居环境预测及矿产资源勘探;小尺度古地理研究为在一个沉积体系内,以万年或十几万年为时间单元,研究亚/微环境的特征、分布、变迁及相应的小规模地表作用过程,用于人类居住环境预测以及矿产资源评价与开发.未来的古地理学应进一步发展不同尺度古地理参数的多信息定量解译方法,创新不同尺度古地理的智能化重建技术,深化不同尺度古地理的成因机制研究,建立不同尺度古地理对矿产资源分布的控制作用模式,加强多尺度古地理的协同研究.

Palaeogeographic units on the Earth's surface exhibit a hierarchical structure,however,their connotations,research significance,reconstruction scales,and methodologies remain unclear,hindering the coordinated development of palaeogeography.Each palaeogeographic unit is a palaeo-geographic unit with specific climatic,hydrological,and ecological characteristics.Based on the relative size and formation of landforms,palaeogeographic units are divided into three levels:large,medium,and small,correspondingly classifying palaeogeographic research scales into three levels.Large-scale palaeogeographic research investigates the spatiotemporal distribution and multi-sphere interactions of large-scale palaeogeographic units(oceans,continents,and large-scale geomorphic undulations within them)over millions to tens of millions of years.This research is conducted globally and across tectonic plates(or basins),aiming to predict habitable Earth and prospective areas for mineral resources.Medium-scale palaeogeographic research focuses on the characteristics,distribution,evolution,and associated surface processes of medium-scale palaeogeographic units(geomorphic units between large-scale geomorphic undulations and sub-environments)within a large geomorphic unit(such as a basin).It operates on timescales of hundreds of thousands of years and serves to predict habitable region and guide mineral resource exploration.Small-scale palaeogeographic research examines the characteristics,distribution,changes,and corresponding small-scale surface processes of sub-/micro-environments within a sedimen-tary system.This research covers timescales of tens to hundreds of thousands of years and aims to predict human habitable locality and to evaluate and develop mineral resources.Future palaeogeography should further develop multi-information quantitative interpretation methods for multi-scale palaeogeographic parameters,innovate intelligent reconstruction technologies of multi-scale palaeogeography,deepen the understanding of the formation mechanisms across different scales,establish models that explain how palaeogeography controls mineral resource distribution at various scales,and enhance collaborative research on multi-scale palaeogeography.

吴胜和;孙龙德;鲍志东;邵龙义;吴因业;郑秀娟

油气资源与工程全国重点实验室,中国石油大学(北京),北京 102249||中国石油大学(北京)地球科学学院,北京 102249多资源协同陆相页岩油绿色开采全国重点实验室,黑龙江大庆 163712||中国石油天然气集团有限公司,北京 100007中国石油大学(北京)地球科学学院,北京 102249中国矿业大学(北京)地球科学与测绘工程学院,北京 100083中国石油勘探开发研究院,北京 100083中国石油大学(北京)期刊社,北京 102249

天文与地球科学

古地理学多尺度宜居地球矿产资源

palaeogeographymultiscalehabitable Earthmineral resources

《古地理学报》 2026 (3)

843-864,22

国家自然科学基金(编号:42272110,41772101)资助.[Financially supported by the National Natural Science Foundation of China(Nos.42272110,41772101)]

10.7605/gdlxb.2026.009

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