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川西龙门山前陆盆地南段前缘砾石层成因及青衣江演化过程:基于宇宙成因核素26Al/10Be埋藏年龄

周游 李斌 吴中海 左嘉梦 邹任洲 郑丽萍

现代地质2024,Vol.38Issue(4):1121-1133,13.
现代地质2024,Vol.38Issue(4):1121-1133,13.DOI:10.19657/j.geoscience.1000-8527.2023.106

川西龙门山前陆盆地南段前缘砾石层成因及青衣江演化过程:基于宇宙成因核素26Al/10Be埋藏年龄

Origin of the Gravel Layer and Evolution of the Qingyi River in Front of the Southern Longmen Shan Foreland Basin:Insights from the Burial Age of Cosmogenic Nuclides 26Al/10Be

周游 1李斌 1吴中海 2左嘉梦 3邹任洲 4郑丽萍5

作者信息

  • 1. 韩山师范学院地理科学与旅游学院·潮菜学院,广东潮州 521041
  • 2. 中国地质科学院地质力学研究所,北京 100081
  • 3. 山东省水利勘测设计院有限公司,山东济南 250013
  • 4. 中国建筑材料工业地质勘查中心广东总队,广东广州 510450
  • 5. 韩山师范学院现代教育技术中心,广东潮州 521041
  • 折叠

摘要

Abstract

Since the Miocene,strong thrust uplift has occurred in the Longmen Shan nappe tectonic belt,resul-ting in the formation of a steep topographic gradient zone.In the foreland region,ancient alluvial fans composed of gravels have been widely developed,primarily including the Mingshan-Qionglai(MQ)and Danling-Simeng(DS)gravel layers.These layers,deposited by the ancient Qingyi River,are ideal for exploring the river's evo-lution and the paleoenvironmental changes in this region.We conducted field investigation in the Longmen Shan Foreland region and performed cosmogenic nuclide 26Al/10Be dating analysis on the MQ and DS gravel layers.The analysis indicates that the burial age of the MQ gravel layer is 0.608,9±0.018,7 Ma,and the burial age of the DS gravel layer is 0.218,0±0.094,1 Ma.Therefore,we conclude that the MQ gravel layer formed in the late Early Pleistocene to early Middle Pleistocene(Q31-Q12),and the DS gravel layer formed in the Middle Pleistocene(Q22).Combing previous research results,the two gravel layers correspond to the δ180 curve of deep-sea ice core and the sequence curve of Chinese loess,indicating they formed during a warm interglacial period.Based on statistical analysis of gravel composition,size,orientation,and paleoflow directions in the re-gion,three major diversion events have been identified in the Qingyi River system.In the early stage,the Qingyi River flowed from Ya'an in a north-northeast direction towards Jianshan.With the uplift of the Xiongpo anticline and the continued uplift of the Mingshan Qionglai terraces,the Qingyi River,which initially flowed from the southwest-north to the northeast,was forced to cut through the Xiongpo anticline and divert southeast at Caoba.

关键词

宇宙成因核素定年/名邛砾石层/丹思砾石层/青衣江

Key words

cosmogenic nuclide/Mingshan Qionglai gravel bed/Danling-Simeng gravel bed/the Qingyi river

分类

天文与地球科学

引用本文复制引用

周游,李斌,吴中海,左嘉梦,邹任洲,郑丽萍..川西龙门山前陆盆地南段前缘砾石层成因及青衣江演化过程:基于宇宙成因核素26Al/10Be埋藏年龄[J].现代地质,2024,38(4):1121-1133,13.

基金项目

韩山师范学院2021年教授博士启动项目(QD202106). (QD202106)

现代地质

OA北大核心CSTPCD

1000-8527

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