The sedimentary environment and main controlling factors of organic matter enrichment of Carboniferous-Permian marine-continental transitional shale in Kaiping syncline-Reference-Cited by-同舟云学术

The sedimentary environment and main controlling factors of organic matter enrichment of Carboniferous-Permian marine-continental transitional shale in Kaiping syncline

Published:2024-07-12 Issue: Volume: Page:1-21
ISSN:1091-6466
Container-title:Petroleum Science and Technology
language:en
Short-container-title:Petroleum Science and Technology

Author:

Wang Yang¹²^ORCID,Zhang Hanyu¹²,Chen Haoran¹²,Zhu Yanming¹²,Yang Jinghui¹²,Zhang Yunsheng¹²,Dou Kailong¹²,Wang Zhixuan¹²

Affiliation:

1. Key Laboratory of Coalbed Methane Resources and Reservoir Formation Process, Ministry of Education, China University of Mining and Technology, Xuzhou, Jiangsu, China

2. School of Resources and Geoscience, China University of Mining and Technology, Xuzhou, Jiangsu, China

Funder

National Natural Science Foundation of China

Fundamental Research Funds for the Central Universities

National Key R&D Program of China

National Key Research and Development Program of China

Publisher

Informa UK Limited

Link

https://www.tandfonline.com/doi/pdf/10.1080/10916466.2024.2377333

Reference37 articles.

1. Sedimentary Corg:P ratios, paleocean ventilation, and Phanerozoic atmospheric pO2

2. Paleoproductivity and paleoredox condition of the Huai Hin Lat Formation in northeastern Thailand

3. Mineralogy and geochemistry of the Middle Permian Pingdiquan Formation black shales on the eastern margin of the Junggar Basin, north‐west China: Implications for palaeoenvironmental and organic matter accumulation analyses

4. Stratigraphic classification of ancient lakes: Balancing tectonic and climatic controls

5. Differential enrichment mechanism of organic matters in the marine-continental transitional shale in northeastern Ordos Basin, China: Control of sedimentary environments