Energy Exploration & Exploitation (Nov 2020)

Quality, hydrocarbon generation, and expulsion of the Eocene Enping Formation source rocks in the Wenchang Depression, western Pearl River Mouth Basin, South China Sea

  • Jinheng Li,
  • Dongxia Chen,
  • Lu Chang,
  • Guangjie Xie,
  • Xuebin Shi,
  • Fuwei Wang,
  • Wenhao Liao,
  • Ziyi Wang

DOI
https://doi.org/10.1177/0144598720915583
Journal volume & issue
Vol. 38

Abstract

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Recently, increasing numbers of oil and gas reservoirs have been discovered in the Wenchang Depression, western Pearl River Mouth Basin, South China Sea, revealing prospects for hydrocarbon exploration. The Enping Formation (E 3 e) is a key target layer for the development of source rocks. However, previous work has only focused on lacustrine swamp source rocks of E 3 e in the Wenchang A Sag, without a systematic study of shallow lacustrine source rocks. In this study, the quality of E 3 e shallow lacustrine source rocks is reevaluated, and the hydrocarbon generation and expulsion characteristics are analyzed using relevant geological data and constructing a conceptual model. The results show that the E 3 e 2 source rocks have greater thickness (50–600 m) and similar organic matter abundance (0.5–2.5%) compared with the E 3 e 1 source rocks (50–500 m and 0.5–2.5%). On the whole, the E 3 e source rocks were deposited in the continental environment and are dominated by Type II and Type III kerogen. Meanwhile, the E 3 e source rocks of the Wenchang A Sag are in the stage of mature to over mature, while those of the Wenchang B Sag are in the stage of low mature. Vertically, the hydrocarbon generation potential of the E 3 e 2 source rocks is greater than E 3 e 1 . Also, the cumulative hydrocarbon production of steep slope in the Wenchang A Sag is larger than that in the Wenchang B Sag. In addition, the corresponding vitrinite reflectances of hydrocarbon expulsion threshold and peak are 0.72 and 0.96%, respectively. Horizontally, four hydrocarbon generation and expulsion centers were mainly concentrated in different subsags of the Wenchang A and B Sags for E 3 e. The maximum values of hydrocarbon generation and expulsion intensity for E 3 e 1 are 1500 × 10 4 t/km 2 and 1000 × 10 4 t/km 2 , respectively, while those for E 3 e 2 are 1800 × 10 4 t/km 2 and 1200 × 10 4 t/km 2 , respectively, with the expulsion efficiency of 75%.