Thermal-history reconstruction of the Baiyun Sag in the deep-water area of the Pearl River Mouth Basin, northern South China Sea

Abstract

The Baiyun Sag, located in the deep-water area of the northern South China Sea, is the largest and deepest subbasin in the Pearl River Mouth Basin and one of the most important hydrocarbon-accumulation depression areas in China. Thermal history is widely thought to be of great importance in oil and gas potential assessment of a basin as it controls the timing of hydrocarbon generation and expulsion from the source rock. In order to unravel the paleo-heat flow of the Baiyun Sag, we first analyzed tectonic subsidence of 55 pseudo-wells constructed based on newly interpreted seismic profiles, along with three drilled wells. We then carried out thermal modeling using the multi-stage finite stretching method and calibrated the results using collected present-day vitrinite reflectance data and temperature data. Results indicate that the first and second heating of the Baiyun Sag after 49 Ma ceased at 33.9 Ma and 23 Ma. Reconstructed average basal paleo-heat flow values at the end of the rifting periods are ~57.7–86.2 mW/m² and ~66.7–97.3 mW/m², respectively. Following the last heating period at 23 Ma, the study area has undergone a persistent thermal attenuation phase, and basal heat flow has cooled down to ~64.0–79.2 mW/m² at present.

Keywords

thermal history / tectonic subsidence / Baiyun Sag / deep-water area / South China Sea

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Acknowledgements

Research in this paper was supported by the National Natural Science Foundation of China (Grant No. 41602251), the Chinese Postdoc Fund, No.58 General Fund, 2015 (No. 2015M582636) and the Research Fund for New Teachers of Xi’an Jiaotong University. We are grateful to CNOOC Research Institute for providing the seismic profiles. We also thank anonymous reviewers for their careful and insightful suggestions on the paper.

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