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    Volume 36 Issue 3
    May  2011
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    WU Huai-chun, ZHANG Shi-hong, FENG Qing-lai, FANG Nian-qiao, YANG Tian-shui, LI Hai-yan, 2011. Theoretical Basis, Research Advancement and Prospects of Cyclostratigraphy. Earth Science, 36(3): 409-428. doi: 10.3799/dqkx.2011.045
    Citation: WU Huai-chun, ZHANG Shi-hong, FENG Qing-lai, FANG Nian-qiao, YANG Tian-shui, LI Hai-yan, 2011. Theoretical Basis, Research Advancement and Prospects of Cyclostratigraphy. Earth Science, 36(3): 409-428. doi: 10.3799/dqkx.2011.045

    Theoretical Basis, Research Advancement and Prospects of Cyclostratigraphy

    doi: 10.3799/dqkx.2011.045
    • Received Date: 2010-11-01
    • Publish Date: 2011-05-01
    • The research on cyclostratigraphy has made great progress over the past 30 years, and it has contributed to the understanding and solutions of numerous scientific problems in the field of Earth Science. Now cyclostratigraphy has been defined as "the subdiscipline of stratigraphy that deals with the identification, characterization, correlation, and interpretation of cyclic variations in the stratigraphic record and, in particular, with their application in geochronology by improving the accuracy and resolution of time-stratigraphic frameworks". The lithological, facies, geophysical and geochemical parameters (i.e., paleoclimate proxies), which can reflect paleoclimate fluctuations, have been adopted extensively in the cyclostratigraphy analysis. A set of methods, including characterization of lithological combination, power spectral analysis, evolutive power spectral analysis, wavelet analysis, filtering and tuning, have been developed to identify the Milankovitch cycles and establish high-resolution astronomical time scales. Some excellent cyclostratigraphy results have been obtained from loess deposits of northern China, Neogene marine deposits in South China Sea, Paleozoic marine sections, and some Meso-Neozoic terrestrial basins by Chinese scholars. We may get some important results if we can carry out cyclostratigraphy research on the Cretaceous terrestrial deposits in Songliao basin, northeastern China, and Lopingian-Midddle Triassic marine sections in South China.

       

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