Hydrocarbon generation in source rocks with low organic matter as the primary mechanism for overpressure development: a case study from the Yinggehai Basin, South China Sea

Zhang, Xuyou, Fan, Caiwei, Alves, Tiago M. ORCID: https://orcid.org/0000-0002-2765-3760, Omosanya, Kamaldeen O.L, Tao, Ze, Wu, Yunpeng, Liu, Aiqun, Guo, Xiaowen and Huang, Yahao 2025. Hydrocarbon generation in source rocks with low organic matter as the primary mechanism for overpressure development: a case study from the Yinggehai Basin, South China Sea. Journal of the Geological Society , jgs2024-157. 10.1144/jgs2024-157 Item availability restricted.

PDF - Accepted Post-Print Version Restricted to Repository staff only until 19 August 2026 due to copyright restrictions. Download (3MB)

Abstract

Overpressure is developed in both the reservoirs and source rocks of the Huangliu Formation, with pressure coefficients reaching up to 2.31. This study investigates the mechanisms responsible for overpressure in the source rocks of the Huangliu Formation and reconstructs their temporal evolution. Overpressured mudstones have anomalously high acoustic velocity and low resistivity values. However, the absence of low-density values indicates that disequilibrium compaction is not responsible for the observed overpressure. The source rocks in this formation predominantly contain type III kerogen (gas-prone), with total organic carbon(TOC) values ranging from 0.4% to 2.56% and an average value of 0.79%. Overpressured mudstones are buried at depths above 3300-4300m, and subjected to formation temperatures ranging from 135℃ to 200℃ and the relevant vitrinite reflectance (R o ) of 0.7%-1.57%. Models of maturity and hydrocarbon generation history show that mudstones started to become overpressured at 3.5 Ma and that pore pressure is still increasing. This study provides new insights revealing that hydrocarbon generation, rather than disequilibrium compaction, is the primary mechanism driving the overpressure development despite of the low-organic matter content of the source rocks.

Item Type:	Article
Date Type:	Published Online
Status:	In Press
Schools:	Schools > Earth and Environmental Sciences
Additional Information:	License information from Publisher: LICENSE 1: URL: https://www.geolsoc.org.uk/publications/lyell-collection/user-license-1-1, Start Date: 2025-08-19 LICENSE 2: URL: https://www.geolsoc.org.uk/publications/lyell-collection/user-license-1-2, Start Date: 2026-08-19
Publisher:	The Geological Society
ISSN:	0016-7649
Date of First Compliant Deposit:	19 September 2025
Date of Acceptance:	28 July 2025
Last Modified:	19 Sep 2025 15:00
URI:	https://orca.cardiff.ac.uk/id/eprint/180882

Actions (repository staff only)

Edit Item