Volume 37 Issue 3
May  2012
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LIU Yang, WU Huai-chun, ZHANG Shi-hong, FANG Nian-qiao, JIANG Zheng-long, YANG Tian-shui, 2012. Cyclostratigraphy Research on the Hanjiang-Wanshan Formations in Zhuyi Depression, Pearl River Mouth Basin. Earth Science, 37(3): 411-423. doi: 10.3799/dqkx.2012.049
Citation: LIU Yang, WU Huai-chun, ZHANG Shi-hong, FANG Nian-qiao, JIANG Zheng-long, YANG Tian-shui, 2012. Cyclostratigraphy Research on the Hanjiang-Wanshan Formations in Zhuyi Depression, Pearl River Mouth Basin. Earth Science, 37(3): 411-423. doi: 10.3799/dqkx.2012.049

Cyclostratigraphy Research on the Hanjiang-Wanshan Formations in Zhuyi Depression, Pearl River Mouth Basin

doi: 10.3799/dqkx.2012.049
  • Received Date: 2011-03-21
    Available Online: 2021-11-09
  • Publish Date: 2012-05-01
  • Spectral analysis and continuous wavelet analysis were conducted on the natural gamma ray logging data from the Middle Miocene-Pliocene Hanjiang, Yuehai and Wanshan formations of well HZ0811 and HZ1811, which locate at northern Huizhou depression and Huilu low uplift at Zhuyi depression, respectively. Significant Milankovitch sedimentary cycles were identified, and "floating" astronomical time scales of well HZ0811 and HZ1811 were established through Gaussian band filtering of short eccentricity signals. The Wanshan, Yuehai and Hanjiang formations record 35, 56 and 64 short eccentricity cycles, which indicate the duration of Wanshan, Yuehai and Hanjiang formations can be estimated as 3.5, 5.6 and 6.4 Ma, respectively. The sedimentary rate of Hanjiang-Wanshan formations of well HZ0811 and HZ1811 were calculated according to floating astronomical time scale. The variations of sedimentary rate indicate significant 1.0 Ma and 0.4 Ma cyclicities, which may be related to the sea level change controlled by long eccentricity cycles.

     

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