0.2 Ma or 1.2 Ma? Timing of the Linking of the Middle and Lower Reaches of the Yellow River Inferred From Loess‐Palaeosol Sequences-Reference-Cited by-同舟云学术

0.2 Ma or 1.2 Ma? Timing of the Linking of the Middle and Lower Reaches of the Yellow River Inferred From Loess‐Palaeosol Sequences

Author:

Chen Qu¹^ORCID,Liu Xiuming²³,Zhao Guoyong⁴,Jia Jia¹,Ye Wei¹,LÜ Bin²,Meadows Michael¹⁵⁶^ORCID,Guan Jueqi⁷

Affiliation:

1. College of Geography and Environmental Sciences Zhejiang Normal University Jinhua China

2. State Key Laboratory for Subtropical Mountain Ecology of the Ministry of Science and Technology and Fujian Fujian Normal University Fuzhou China

3. Department of Earth and Environmental Sciences Macquarie University Sydney NSW Australia

4. School of Geographical Sciences Xinyang Normal University Xinyang China

5. Department of Environmental and Geographical Science University of Cape Town Rondebosch South Africa

6. School of Geographical and Oceanographic Sciences Nanjing University Nanjing China

7. Department of Educational Technology Zhejiang Normal University Jinhua China

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

Reference58 articles.

2. Major element geochemical characteristics of Mangshan loess since L5 and its implications for provenance;Chen L.;Quaternary Sciences,2017

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2. 黄河形成于何时?;Earth Science-Journal of China University of Geosciences;2024