Enrichment Mechanism of Organic Matter in the Marine-Continental Transitional Shale of the Taiyuan Formation in Ordos Basin, China: Control of the Paleoenvironment.
- DOI
- 10.1021/acsomega.5c00925
- Published
- 2025 Jun 3
- Container
- ACS omega
- Publisher
- Not recorded
- Open access
- yes
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Cite this work
BibTeX
@article{allodium:10.1021/acsomega.5c00925,
title = {Enrichment Mechanism of Organic Matter in the Marine-Continental Transitional Shale of the Taiyuan Formation in Ordos Basin, China: Control of the Paleoenvironment.},
author = {He Z and Yang M and Wang L and Lu J and Wang Y and Peng X and Shao L},
year = {2025},
journal = {ACS omega},
doi = {10.1021/acsomega.5c00925},
url = {https://doi.org/10.1021/acsomega.5c00925}
}RIS
TY - JOUR TI - Enrichment Mechanism of Organic Matter in the Marine-Continental Transitional Shale of the Taiyuan Formation in Ordos Basin, China: Control of the Paleoenvironment. AU - He Z AU - Yang M AU - Wang L AU - Lu J AU - Wang Y AU - Peng X AU - Shao L PY - 2025 JO - ACS omega DO - 10.1021/acsomega.5c00925 UR - https://doi.org/10.1021/acsomega.5c00925 ER -
APA
Z, H., M, Y., L, W., J, L., Y, W., X, P., & L, S. (2025). Enrichment Mechanism of Organic Matter in the Marine-Continental Transitional Shale of the Taiyuan Formation in Ordos Basin, China: Control of the Paleoenvironment.. ACS omega. https://doi.org/10.1021/acsomega.5c00925
Source records
- pubmed · retrieved 2026-09-25T19:27:16.495Z