The Sources and Transport Dynamics of Eolian Sediments in the NE Tibetan Plateau Since 6.7 Ma-Reference-Cited by-同舟云学术

The Sources and Transport Dynamics of Eolian Sediments in the NE Tibetan Plateau Since 6.7 Ma

Published:2020-02-29 Issue:3 Volume:21 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Li Xiaomiao¹,Peng Tingjiang¹^ORCID,Ma Zhenhua¹,Li Meng¹,Li Peiye¹,Feng Zhantao¹,Guo Benhong¹,Yu Hao¹,Ye Xiyan¹,Zhang Jun¹,Song Chunhui²^ORCID,Li Jijun¹³

Affiliation:

1. MOE Key Laboratory of Western China's Environmental Systems, College of Earth and Environmental SciencesLanzhou University Lanzhou China

2. School of Earth Sciences and Key Laboratory of Western China's Mineral Resources of Gansu ProvinceLanzhou University Lanzhou China

3. College of Geographical ScienceNanjing Normal University Nanjing China

Funder

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GC008682

Reference98 articles.

1. Evolution of Asian monsoons and phased uplift of the Himalaya–Tibetan plateau since Late Miocene times

2. Significantly warmer Arctic surface temperatures during the Pliocene indicated by multiple independent proxies

3. Eocene Tibetan plateau remnants preserved in the northwest Himalaya

4. Quaternary dust source variation across the Chinese Loess Plateau

5. Pliocene Warmth, Polar Amplification, and Stepped Pleistocene Cooling Recorded in NE Arctic Russia

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