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Reconstructing the Climatic–Oceanic Environment and Exploring the Enrichment Mechanism of Organic Matter in the Black Shale across the Late Ordovician–Early Silurian Transition on the Upper Yangtze Platform Using Geochemical Proxies
[Image: see text] Black shale deposited in the transitional period from the Late Ordovician to Early Silurian is the most important source rock and shale gas reservoir in the Yangtze region of South China. However, the source of these sediments is still controversial. In this paper, the changes in t...
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| Pubblicato in: | ACS Omega |
|---|---|
| Autori principali: | , , , , , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
American Chemical Society
2020
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| Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7594159/ https://ncbi.nlm.nih.gov/pubmed/33134707 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1021/acsomega.0c03912 |
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