地学前缘 ›› 2023, Vol. 30 ›› Issue (4): 389-404.DOI: 10.13745/j.esf.sf.2022.12.52

• 非主题来稿选登 • 上一篇    下一篇

现代河流扇的全球分布、类型及控制因素

张元福1(), 王敏2, 张森1, 孙世坦1, 李鑫鑫1, 袁晓冬1, 黄云英1, 张晓晗1   

  1. 1.中国地质大学(北京) 能源学院, 北京 100083
    2.中国石油勘探开发研究院, 北京 100083
  • 收稿日期:2022-09-06 修回日期:2023-01-06 出版日期:2023-07-25 发布日期:2023-07-07
  • 作者简介:张元福(1979-),男,博士,教授,博士生导师,主要从事沉积学理论及油气储集层的研究工作。E-mail: zyf@cugb.edu.cn
  • 基金资助:
    国家科技重大专项“陆相深水储集体成因与地质评价新方法”(2017ZX05009-002)

Modern fluvial fans: Global distribution, fan types and controlling factors

ZHANG Yuanfu1(), WANG Min2, ZHANG Sen1, SUN Shitan1, LI Xinxin1, YUAN Xiaodong1, HUANG Yunying1, ZHANG Xiaohan1   

  1. 1. School of Energy Resources,China University of Geosciences (Beijing), Beijing 100083, China
    2. PetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083, China
  • Received:2022-09-06 Revised:2023-01-06 Online:2023-07-25 Published:2023-07-07

摘要:

扇研究一直是沉积学中充满活力的研究主题,河流扇是扇研究的重要组成部分。近年来,河流扇研究引起了诸多学者关注,多种相关术语体系并行。针对上述问题,我们建立了一个融合383个全球现代河流扇沉积数据集,统计分析各类数据达8 400条。基于数据集,我们首次掌握了现代河流扇的全球分布,划分了河流扇的主要类型,明确了扇体形成、发育的控制因素。其中,河流扇的全球分布具备明显的纬度分带和地域分区特征:从纬度上看,主要发育在北纬30°~50°(49.5%);从地域上看,主要分布在亚洲中部及中国西部(50.1%)。根据地形限制和河道摆动情况,可以把河流扇分为非限制迭进型、非限制摆动型、限制迭进型和限制摆动型4种形态类型。河流扇主要在干旱、半干旱条件下形成,受局部构造条件、气候以及物源供给控制。扇体内部建造以河流作用为主,从扇体顶点到远端呈现出明显的异质性。扇体的面积直接受控于纬度、温度、坡度、集水区面积、区域年降雨量和山前距离等因素。随着研究的进一步深入,河流扇将在沉积学、地质灾害防治、石油勘探,甚至行星际沉积学等方面发挥重要作用。

关键词: 河流扇, 控制因素, 河流扇类型, 河流扇数据集

Abstract:

Fluvial fans are an important topic in sedimentology. As fan research attracts more attention in recent years, various fan terminology systems are being used in parallel, but there lacks an independent terminology system for fluvial fans. To address this issue, we constructed a sediment dataset containing sediments from 383 modern fluvial fans across the globe, with 8400 data analyzed using statistical method. For the first time, based on the dataset, we obtained the global distribution of modern fluvial fans, delineated the main fan types, and clarified the controlling factors of fan formation and development. The global distributions of fluvial fans show obvious latitudinal and geographical zonation, with 49.5% fans distributed between 30°N-50°N and 50.1% in central Asia and western China. According to the topographic and river swing conditions, fluvial fans can be divided into four types: unrestricted superposition, unrestricted swing, restricted superposition and restricted swing. Fluvial fans are mainly formed under arid and semi-arid climates, controlled by local tectonic conditions, climate and material source supply. Fluvial sedimentation is dominant in fluvial fans which show obvious heterogeneity from the apex to the end of the fan. The area of a fluvial fan is controlled by latitude, temperature, slope, catchment area, annual rainfall and apex-to-mountain distance. With more in-depth research, fluvial fans will play an increasingly important role in sedimentology, geological disaster prevention, oil exploration, and even in interplanetary sedimentology.

Key words: fluvial fan, controlling factors, fluvial fan type, dataset of fluvial fan

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