Accumulation and Quantitative Assessment of Terrigenous Organic Matter in Upper Oligocene to Lower Miocene Marine Source Rocks of the Qiongdongnan Basin-Reference-Cited by-同舟云学术

Accumulation and Quantitative Assessment of Terrigenous Organic Matter in Upper Oligocene to Lower Miocene Marine Source Rocks of the Qiongdongnan Basin

Published:2024-05-16 Issue:21 Volume:9 Page:22903-22922
ISSN:2470-1343
Container-title:ACS Omega
language:en
Short-container-title:ACS Omega

Author:

Zhang Ziming¹²³^ORCID,Hou Dujie¹²³^ORCID,Xu Changgui⁴,Wu Keqiang⁵,You Li⁵,Cheng Xiong¹²³^ORCID,Yan Xiaze¹²³,Chen Weihe¹²³

Affiliation:

1. School of Energy Resources, China University of Geosciences, Beijing 100083, China

2. Key Laboratory of Marine Reservoir Evolution and Hydrocarbon Accumulation Mechanism, Ministry of Education, Beijing 100083, China

3. Beijing Key Laboratory of Unconventional Natural Gas Geological Evaluation and Development Engineering, Beijing 100083, China

4. China National Offshore Oil Corporation, Beijing 100010, China

5. China National Offshore Oil Corporation, Hainan, Haikou 570300, China

Funder

National Natural Science Foundation of China

Publisher

American Chemical Society (ACS)

Link

https://pubs.acs.org/doi/pdf/10.1021/acsomega.4c01777

Reference57 articles.

1. Palaeovegetation variation in response to the late Oligocene-early Miocene East Asian summer monsoon in the Ying-Qiong Basin, South China Sea

2. Paleoenvironment and Its Control of the Formation of Oligocene Marine Source Rocks in the Deep-Water Area of the Northern South China Sea

3. Evolutions of sedimentary facies and palaeoenvironment and their controls on the development of source rocks in continental margin basins: A case study from the Qiongdongnan Basin, South China Sea

4. Paleoenvironment and Controlling Factors of Oligocene Source Rock in the Eastern Deep-Water Area of the Qiongdongnan Basin: Evidences from Organic Geochemistry and Palynology

5. Biomarkers reveal the terrigenous organic matter enrichment in the late Oligocene—early Miocene marine shales in the Ying-Qiong Basin, South China Sea