地理科学 ›› 2021, Vol. 41 ›› Issue (10): 1862-1872.doi: 10.13249/j.cnki.sgs.2021.10.018
胡春生1,2(), 田景梅1,2, 何成邦1,2, 周迎秋1,2, 徐光来1,2
收稿日期:
2020-10-11
修回日期:
2021-05-20
出版日期:
2021-10-25
发布日期:
2021-12-08
作者简介:
胡春生(1978-),男,安徽无为人,副教授,主要从事河流地貌与环境研究。E-mail: huchsh03@ahnu.edu.cn
基金资助:
Hu Chunsheng1,2(), Tian Jingmei1,2, He Chengbang1,2, Zhou Yingqiu1,2, Xu Guanglai1,2
Received:
2020-10-11
Revised:
2021-05-20
Online:
2021-10-25
Published:
2021-12-08
Supported by:
摘要:
基于前期研究工作成果和外部环境变化因素分析,探讨了青弋江发育原因及其与长江贯通的关系。研究表明:① 昆黄运动可能在长江中下游地区产生了区域构造响应,导致研究区断层被激活而发生了较大幅度的断块抬升运动,进而为青弋江发育提供了下切驱动力,驱动了青弋江发育;② 东亚夏季风在约1.3 Ma和约0.9 Ma发生的2次显著阶段性减弱事件,引起区域降水量显著增加,进而为青弋江发育提供了下切媒介和持续水流,控制了青弋江发育年代;③ 青弋江发育与长江贯通可能都是昆黄运动区域构造响应与东亚夏季风强度阶段性减弱共同作用的结果,并且长江贯通后所形成的新局部侵蚀基准面也可能促进了青弋江发育,因此青弋江发育年代在一定程度上能反映长江贯通年代。
中图分类号:
胡春生, 田景梅, 何成邦, 周迎秋, 徐光来. 黄山北麓青弋江发育原因及其与长江贯通的关系[J]. 地理科学, 2021, 41(10): 1862-1872.
Hu Chunsheng, Tian Jingmei, He Chengbang, Zhou Yingqiu, Xu Guanglai. Development Causes of the Qingyijiang River on the Northern Piedmont of the Huangshan Mountain and Its Relationship with the Channelization of the Yangtze River[J]. SCIENTIA GEOGRAPHICA SINICA, 2021, 41(10): 1862-1872.
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