Origin and Formation Mechanism of the Late Permian Black Siliceous Rocks in the Lower Yangtze Region-Reference-Cited by-同舟云学术

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Origin and Formation Mechanism of the Late Permian Black Siliceous Rocks in the Lower Yangtze Region

Published:2024-04-11 Issue:16 Volume:9 Page:17848-17859
ISSN:2470-1343
Container-title:ACS Omega
language:en
Short-container-title:ACS Omega

Author:

Gao Xue¹²,Liu Qi³,Fang Chaogang⁴^ORCID,Guo Yinghai¹

Affiliation:

1. School of Resources and Geosciences, China University of Mining and Technology, 221116 Xuzhou, China

2. Nanjing City Vocational college, 211200 Nanjing, China

3. Sichuan Liwu Copper Co., Ltd., 610091 Chengdu, China

4. Nanjing Center, China Geological Survey, 210016 Nanjing, China

Funder

China Geological Survey, Ministry of Natural Resources

National Natural Science Foundation of China

Publisher

American Chemical Society (ACS)

Link

https://pubs.acs.org/doi/pdf/10.1021/acsomega.3c08384

Reference89 articles.

1. A mid-Permian chert event: widespread deposition of biogenic siliceous sediments in coastal, island arc and oceanic basins

2. Growth and demise of Permian biogenic chert along northwest Pangea: evidence for end-Permian collapse of thermohaline circulation

3. Sedimentary environments of the Middle Permian phosphorite–chert complex from the northeastern Yangtze platform, China; the Gufeng Formation: a continental shelf radiolarian chert

4. Geochemical evidence for submarine hydrothermal origin of the Middle-Upper Permian chert in Laibin of Guangxi, China

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