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Volume 11 Issue 1
Mar 2000
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Fengjun Nie, Sitian Li, Xinong Xie, Hua Wang, Weilin Zhu, Keqiang Wu. Study on Basin-Filling and Reservoir Sedimentology of Zhu Ⅲ Depression of Pearl River Mouth Basin, South China Sea. Journal of Earth Science, 2000, 11(1): 37-46.
Citation: Fengjun Nie, Sitian Li, Xinong Xie, Hua Wang, Weilin Zhu, Keqiang Wu. Study on Basin-Filling and Reservoir Sedimentology of Zhu Ⅲ Depression of Pearl River Mouth Basin, South China Sea. Journal of Earth Science, 2000, 11(1): 37-46.

Study on Basin-Filling and Reservoir Sedimentology of Zhu Ⅲ Depression of Pearl River Mouth Basin, South China Sea

Funds:

National Natural Science Foundation of China 49732005-01

  • Received Date: 19 Dec 1999
  • Rev Recd Date: 15 Jan 2000
  • Through basin-filling analysis, one coarsening-upward and two fining-upward sequences have been identified in Zhu Ⅲ depression. In accondance with the general model proposed by Ravnas and Steel (1998), the basin-filling has two large cycles—rift (sediment-balanced and -overfilled) and postrift (sedimentunderfilled and starved). During the rifting process, the rifted lake developed through three stages: early, climax and late. The sedimentary characteristics of reservoir rocks show that barrier bar, lagoon and tidal channel facies well developed in Zhuhai Formation; offshore, tidal and barrier bar well developed in Zhujiang Formation. Neighborly, Shenhu, Wenchang and Enping formations deposited in rifted lakes during Paleogene time; Zhujiang Formation deposited in bay, lagoon and shoreface in late Paleogene. Zhujiang and other formations deposited in offshore and open shallow sea to shelf.

     

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