地质论评2024，Vol.70Issue(2)：436-448,13.DOI:10.16509/j.georeview.2023.10.051
长江武汉段天兴洲低滩沉积物粒度端元对河流—风成沙丘沉积环境的指示意义
Fluvial—aeolian dune depositional environment significances from grain-size end-member in low-beach at the head of Tianxing Central-bar in Wuhan section of Yangtze River
摘要
关键词
粒度分布/端元分析/长江天兴洲/河流/风成沙纹/沉积环境Key words
grain-size distribution/end-member analysis/Tianxing Central-bar in Yangtze River/river/aeolian sand-ripple/depositional environment引用本文复制引用
袁瑞,冯文杰,张昌民,赵康,刘家乐,付文俊,王泽宇,孟庆昊,王令辉..长江武汉段天兴洲低滩沉积物粒度端元对河流—风成沙丘沉积环境的指示意义[J].地质论评,2024,70(2):436-448,13.基金项目
本文为国家自然科学基金资助项目(编号:42202113、42130813)的成果.This research is supported by Natural Science Foundation of China(Nos.42202113 and 42130813). （编号:42202113、42130813）
