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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2014  >  36(4): 435-441
Xi Minhong, Zhou Xinghai, Wang Lin, Yu Xuebing. Bioherm developmental mode in deepwater area of Qiongdongnan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(4): 435-441. doi: 10.11781/sysydz201404435
Citation: Xi Minhong, Zhou Xinghai, Wang Lin, Yu Xuebing. Bioherm developmental mode in deepwater area of Qiongdongnan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(4): 435-441. doi: 10.11781/sysydz201404435
shu

Bioherm developmental mode in deepwater area of Qiongdongnan Basin

doi: 10.11781/sysydz201404435

  • SINOPEC Shanghai offshore Oil & Gas Company, Shanghai 200120, China

  • Received Date: 2014-04-01
  • Rev Recd Date: 2014-06-15
  • Publish Date: 2014-07-28
    Abstract
  • The analyses of paleostructure, paleogeographic and sea level changes in the deepwater area of the Qiongdongnan Basin show that Miocene is favorable for bioherm development. The characteristics of sequence stratigraphic structure indicate that both slope platform margin and fault-controlled platform margin generate in the south of the deepwater area, giving birth to bioherm with obviously different evolution features. As to the fault-controlled platform margin, the Mei2 period is the main beach-forming period, and the Mei1 period is the main bioherm-forming period. As to the slope platform margin, both beach and bioherm develop during the Mei2 period, and the bioherm development scale is smaller; while in the Mei1 period, only beach develops.

     

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