Journal of Tropical Oceanography ›› 2014, Vol. 33 ›› Issue (5): 50-59.doi: 10.11978/j.issn.1009-5470.2014.05.007cstr: 32234.14.j.issn.1009-5470.2014.05.007

• Marine Geology • Previous Articles     Next Articles

Uncertainty and parameterization in backstripping of basin subsidence analysis

XIE Hui1, 2, ZHOU Di1, CHEN Guang-hao1, LI Peng-chun1, PANG Xiong3, LI Yuan-ping3, ZHAO Mei-song4   

  1. 1. Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China; 2. University of Chinese Academy of Sciences, Beijing 100049, China; 3. China National Offshore Oil Corporation (CNOOC) China Ltd-Shenzhen, Guangzhou 510240, China; 4. Geological Scientific Research Institute of Shengli Oilfield Co. Ltd., China Petroleum & Chemical Corporation (SINOPEC), Dongying 257000, China.;
  • Received:2014-01-22 Revised:2014-04-14 Online:2014-09-29 Published:2014-09-29

Abstract: Backstripping is an important and widely used method for basin subsidence analysis. Little attention has been paid on the uncertainty of its results. In this paper, we address this issue based on a study of the Baiyun Sag in the Pearl River Mouth Basin. We demonstrated through theoretical analysis and sensitivity tests that the uncertainty in the non-recovery of the basement depth will pass on to all the results of backstripping, but the uncertainty in age only affects the estimations of sedimentary and subsidence rates. Formation lithology influences the selection of porosity and density parameters. The porosity-depth curves of sandstone and shale vary from area to area. Largest uncertainty comes from paleo-water depth, whose error is 100% inherited by the calculated tectonic subsidence. In the slope area, paleo-water depth and lithology vary significantly with locations. Thus, it is essential to use the paleo-water depth and lithology parameters that are variable with locations. The uncertainty in the source data and inappropriate parameters may lead to erroneous results. Caution should be taken when reading published backstripping results. The quality of parameterization needs to be examined before adopting the results.

Key words: backstripping, subsidence analysis, uncertainty, parameters, Baiyun Sag, Pearl River Mouth Basin

CLC Number: 

  • P736