A climate change from icehouse to greenhouse following Huronian glaciation: Evidence from long-term storm deposits of the Paleoproterozoic Hutuo Group in the North China Craton-Reference-Cited by-同舟云学术

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A climate change from icehouse to greenhouse following Huronian glaciation: Evidence from long-term storm deposits of the Paleoproterozoic Hutuo Group in the North China Craton

Published:2024-10 Issue: Volume:274 Page:106289
ISSN:1367-9120
Container-title:Journal of Asian Earth Sciences
language:en
Short-container-title:Journal of Asian Earth Sciences

Author:

Shang Guangrui,Zhai Mingguo,Peng Peng,Miao Peisen,Li Qi

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Reference127 articles.

1. Liquefaction and fluidization structures in Messinian storm deposits (Bajo Segura Basin, Betic Cordillera, southern Spain);Alfaro;Int. J. Earth Sci.,2002

2. The Early Precambrian Geology of Wutaishan;Bai,1986

3. Quantifying climate conditions for the formation of coals and evaporates;Bao;Natl. Sci. Rev.,2023

4. Oxygen overshoot and recovery during the early Paleoproterozoic;Bekker;Earth Planet. Sci. Lett.,2012

5. Evidence for Paleoproterozoic cap carbonates in North America;Bekker;Precambr. Res.,2005

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