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Controlling Factors on Organic Matter Accumulation of Marine Shale across the Ordovician-Silurian Transition in South China: Constraints from Trace-Element Geochemistry
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“The low TOC values usually suggest a shallow, non- stratified, closed lake environment with an oxygenated bottom (Qiu etal.,2021).”
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Metadata
- Authors
- Qiu, Z., Tao, H., Lu, B., Chen, Z., Wu, S., Liu, H., & Qiu, J.
- Affiliations
- Research Institute of Petroleum Exploration and Development (CN)
- Chinese Academy of Sciences (CN)
- Peking University (CN)
- Corresponding author
- Tao, Huifei
- Venue
- Journal of Earth Science
- Published
- 2021-08
- Volume
- 32
- Issue
- 4
- Pages
- 887-900
- ISSN
- 1002-0705 (ISSN-L)
- 1674-487X
- 1867-111X
- OpenAlex
- W3194490640
- Cited by
- 34
- References
- 108
- Citations by year
- 2026: 5 · 2025: 2 · 2024: 4 · 2023: 13 · 2022: 7 · 2021: 3
- FWCI
- 5.07
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Journal of Earth Science (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Geology › Hydrocarbon exploration and reservoir analysis
- Keywords
- organic matter accumulation, marine shale, Ordovician-Silurian transition, trace element geochemistry, terrigenous input, redox conditions, primary productivity, sea-level change, weathering, shale gas, Wufeng Formation, Longmaxi Formation, South China
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- Qiu, Z., Tao, H., Lu, B., Chen, Z., Wu, S., Liu, H., & Qiu, J. (2021). Controlling Factors on Organic Matter Accumulation of Marine Shale across the Ordovician-Silurian Transition in South China: Constraints from Trace-Element Geochemistry. Journal of Earth Science. https://doi.org/10.1007/s12583-020-1359-x