Lithologic Reservoirs ›› 2025, Vol. 37 ›› Issue (5): 166-177.doi: 10.12108/yxyqc.20250515

• PETROLEUM EXPLORATION • Previous Articles    

Source-to-sink system of Paleogene in Huizhou Sag of Pearl River Mouth Basin and its control on reservoir

YAN Yuyang1, XIONG Lianqiao2, HE Youbin1, CHEN Ying2, ZHAO Zhongxiang1, LIU Shengqian1, LUO Jinxiong1, FENG Bin3   

  1. 1. School of Geosciences, Yangtze University, Wuhan 430100, China;
    2. China National Offshore Oil Corporation, Beijing 100028, China;
    3. Changqing Branch, China National Logging Corporation, Xi'an 710000, China
  • Received:2025-02-15 Revised:2025-03-30 Published:2025-09-06

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Abstract: Paleogene tectonic evolution of Huizhou Sag in Pearl River Mouth Basin is complex，and the sourceto-sink elements are variable. Based on data obtained from drilling，seismic，petrographic thin section，detrital zircon geochronology，the source-to-sink system and its control on reservoir was studied. The results show that： （1）Three types of source-to-sink systems developed in Paleogene of Huizhou Sag：the low uplift fault-trough type，the intra-depression transfer zone type，and the extra-depression transfer zone type. The parent rocks of the low uplift fault-trough type source-to-sink system were mainly the granite basement within the basin，transported through the same-direction fault troughs，and developed small-scale braided river deltas. The parent rocks of the intra-depression transfer zone type source-to-sink system were mainly the granite basement，transported via the transfer zone，and developed medium-scale braided river deltas. Affected by the fjord topography，they occasionally superimposed with the adjacent fan deltas sedimentary bodies. The extra-depression transfer zone type source-to-sink system was mainly sourced from the external water system，with a long transport distance and only a small amount of internal source mixing，developed large-scale braided river deltas.（2）The scale and physical properties of reservoirs in the study area are jointly controlled by parent rock composition，transport distance，transport channel morphology，sedimentary facies，and paleogeomorphology of the sedimentary period. （3）There are three types of high-quality reservoirs：the endogenous dissolution type，the mixed-source convergence type，and the low-uplift beach-bar type. The reservoir physical properties of the mixed-source convergence type at the junction of the exogenous transfer zone and the low uplift within the basin are the best.

Key words: source-to-sink system, low uplift fault-trough, intra-depression transfer zone, extra-depression transfer zone, braided river delta, Wenchang Formation, Enping Formation, Paleogene, Huizhou Sag, Pearl River Mouth Basin

CLC Number: 

  • TE122.2
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