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砾石质曲流河探地雷达相刻画及沉积模式研究

韩海波 姚宗全 王威 德勒恰提·加娜塔依 谢宗瑞 汪勇 杨帆 赵文硕

古地理学报2025,Vol.27Issue(4):965-984,20.
古地理学报2025,Vol.27Issue(4):965-984,20.DOI:10.7605/gdlxb.2025.061

砾石质曲流河探地雷达相刻画及沉积模式研究

Ground penetrating radar facies characterization and sedimentary model study of gravelly meandering river

韩海波 1姚宗全 1王威 2德勒恰提·加娜塔依 1谢宗瑞 3汪勇 4杨帆 5赵文硕1

作者信息

  • 1. 新疆大学地质与矿业工程学院,新疆乌鲁木齐 830047||新疆中亚造山带大陆动力学与成矿预测自治区重点实验室,新疆乌鲁木齐 830047
  • 2. 新疆大学地质与矿业工程学院,新疆乌鲁木齐 830047||新疆维吾尔自治区人民政府国家305项目办公室,新疆乌鲁木齐 830000
  • 3. 中国石油新疆油田公司勘探开发研究院,新疆克拉玛依 834000
  • 4. 中国石化胜利油田西部油气勘探项目部,山东东营 257015
  • 5. 中国石油勘探开发研究院,北京 100083
  • 折叠

摘要

Abstract

The meandering river sand bodies exhibit rapid lateral variability and feature complex and heterogeneous internal architectures.In this study,ground-penetrating radar(GPR)was employed in conjunction with a combined plan-view and cross-sectional approach to investigate sedimentary patterns in gravel-dominated meandering river segments of the Hutubi and Irtysh Rivers in Xinjiang.Interpretations of GPR profiles were supported by modern sedimentological observations,UAV imagery,and remote sensing data.Four distinct GPR facies were identified:(1)continuous subparallel low-to-medium amplitude re-flections corresponding to floodplain deposits;(2)continuous flat-topped to convex-based low-to-medium amplitude reflections indicative of abandoned channels;(3)continuous inclined medium-to-high ampli-tude reflections characteristic of point bars;and(4)discontinuous inclined high-amplitude reflections associated with lag deposits.Through an integrated analysis of the vertical and lateral sedimentary evolution and their interactions in gravel-bed meandering systems,a multi-phase depositional model was developed.This model supports the construction of a three-dimensional geological framework,providing refined archi-tectural configurations and quantitative geological information that offer valuable guidance for reservoir pre-diction and modeling in meandering fluvial systems.

关键词

曲流河/探地雷达/沉积微相/沉积模式/呼图壁河/额尔齐斯河/新疆

Key words

gravelly meandering river/GPR(ground penetrating radar)/sedimentary microfa-cies/sedimentary model/Hutubi River/Irtysh River/Xinjiang

分类

天文与地球科学

引用本文复制引用

韩海波,姚宗全,王威,德勒恰提·加娜塔依,谢宗瑞,汪勇,杨帆,赵文硕..砾石质曲流河探地雷达相刻画及沉积模式研究[J].古地理学报,2025,27(4):965-984,20.

基金项目

国家自然科学基金(编号:41902109)和新疆维吾尔自治区天山英才项目(编号:2023TSYCCX0002)联合资助.[Co-funded by the National Natural Science Foundation of China(No.41902109),Tianshan Talent Project of Xinjiang Uygur Autonomous Region(No.2023TSYCCX0002)] (编号:41902109)

古地理学报

OA北大核心

1671-1505

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