Greigite as an Indicator for Salinity and Sedimentation Rate Change: Evidence From the Yangtze River Delta, China-Reference-Cited by-同舟云学术

Greigite as an Indicator for Salinity and Sedimentation Rate Change: Evidence From the Yangtze River Delta, China

Published:2021-03 Issue:3 Volume:126 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J Geophys Res Solid Earth

Author:

Chen Yinglu¹,Zhang Weiguo¹^ORCID,Nian Xiaomei¹^ORCID,Sun Qianli¹,Ge Can²,Hutchinson Simon M.³^ORCID,Cheng Qinzi¹,Wang Feng⁴,Chen Jin¹,Zhao Xuanqi¹

Affiliation:

1. State Key Laboratory of Estuarine and Coastal Research East China Normal University Shanghai China

2. Zhejiang Institute of Hydraulics and Estuary Hangzhou China

3. School of Science, Engineering and Environment University of Salford Greater Manchester UK

4. Guangdong Provincial Key Laboratory of Marine Biotechnology Institute of Marine Sciences Shantou University Shantou China

Funder

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020JB021085

Reference57 articles.

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2. Statistical treatment of fluvial dose distributions from southern Colorado arroyo deposits

3. Magnetic properties of Holocene tidal flats in the Yangtze delta and their paleoenvironmental implications;Bai X. X.;Acta Sedimentologica Sinica,2016

4. C/S method for distinguishing freshwater from marine sedimentary rocks

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