Provenance changes of the Yangtze River Delta sediments since ∼3.6 Ma: Evidence from heavy mineral assemblages and detrital zircon U

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Provenance changes of the Yangtze River Delta sediments since ∼3.6 Ma: Evidence from heavy mineral assemblages and detrital zircon U–Pb ages spectra

Published:2023-10 Issue: Volume:671 Page:33-43
ISSN:1040-6182
Container-title:Quaternary International
language:en
Short-container-title:Quaternary International

Author:

Hao Shefeng,Cheng Yu,Gao Bingfei,Li Xiangqian,Xu Shiyin,Luo Ding

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference75 articles.

1. Physiographic history of the Yangtze;Barbour;Geogr. J.,1936

2. Atlas of Changjiang River Basin,1999

3. Yangtse River sediments and erosion rates from source to sink traced with cosmogenic 10Be: sediments from major rivers;Chappell;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2006

4. Revision on the early Pleistocene lithostratigraphy in the north of the Yangtze River;Cheng;J. Geomechanics,2019

5. Magnetostratigraphy and heavy minerals records of core TZK9 in Subei Basin;Cheng;J. Geomechanics,2016

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